View source for Soil

{{short description|Mixture of organic matter, minerals, gases, liquids, and organisms that together support life}}
{{other uses}}
{{pp-move|small= yes}}

[[File:Stagnogley.JPG|thumb|upright=1.25|Surface-water-[[Gley soil|gley]] developed in [[glacial till]] in [[Northern Ireland]]]]

'''Soil''', also commonly referred to as '''earth''', is a [[mixture]] of [[organic matter]], [[minerals]], [[gas]]es, [[water]], and [[organism]]s that together support the [[life]] of [[plant]]s and [[Soil biology|soil organisms]]. Some scientific definitions distinguish [[dirt]] from soil by restricting the former term specifically to displaced soil.
[[File:EAgronom 4okt2023 L-1120.jpg|thumb|upright|Soil measuring and surveying device]]
Soil consists of a solid collection of [[Mineral|minerals]] and [[organic matter]] (the '''[[soil matrix]]'''), as well as a [[Porosity|porous]] phase that holds [[Soil gas|gases]] (the '''soil atmosphere''') and a liquid phase that holds water and dissolved substances both organic and inorganic, in [[ion]]ic or in [[Molecule|molecular]] form (the '''soil solution''').<ref>{{cite book |last1=Voroney |first1=R. Paul |title=Soil microbiology, ecology and biochemistry |last2=Heck |first2=Richard J. |year=2015 |publisher=[[Elsevier]] |isbn=978-0-12-415955-6 |editor-last=Paul |editor-first=Eldor A. |edition=4th |location=Amsterdam, the Netherlands |pages=15–39 |chapter=The soil habitat |doi=10.1016/B978-0-12-415955-6.00002-5 |access-date=12 November 2025 |chapter-url=https://fr.1lib.sk/book/67708166/606823/soil-microbiology-ecology-and-biochemistry-the-soil-habitat.html }}</ref><ref>{{cite book |last1=Taylor |first1=Sterling A. |url=https://archive.org/details/physicaledapholo0000tayl |title=Physical edaphology: the physics of irrigated and nonirrigated soils |last2=Ashcroft |first2=Gaylen L. |year=1972 |publisher=[[W. H. Freeman and Company|W.H. Freeman]] |isbn=978-0-7167-0818-6 |location=San Francisco, California |access-date=12 November 2025 }}</ref> Accordingly, soil is a [[complex system|complex]] three-[[state of matter|state]] system of solids, liquids, and gases.<ref>{{cite book |last=McCarthy |first=David F. |url=https://fr.1lib.sk/book/3555343/8f031e/essentials-of-soil-mechanics-and-foundations-basic-geotechnics.html |title=Essentials of soil mechanics and foundations: basic geotechnics |year=2014 |publisher=[[Pearson Education|Pearson]] |isbn=978-1-292-03939-8 |edition=7th |location=London, United Kingdom |access-date=12 November 2025 |archive-date=16 October 2022 |archive-url=https://web.archive.org/web/20221016144604/https://fr.b-ok.cc/book/3555343/0f8f97 |url-status=live }}</ref> Soil is a product of several factors: the influence of [[climate]], [[terrain|relief]] (elevation, orientation, and slope of terrain), organisms, and the soil's [[parent material]]s (original minerals) interacting over time.<ref name="Gilluly1975">{{cite book |last1=Gilluly |first1=James |url=https://archive.org/details/principlesofgeol0000gill |title=Principles of geology |last2=Waters |first2=Aaron Clement |last3=Woodford |first3=Alfred Oswald |year=1975 |publisher=[[W. H. Freeman and Company|W.H. Freeman]] |isbn=978-0-7167-0269-6 |edition=4th |location=San Francisco, California |author-link1=James Gilluly |access-date=12 November 2025 }}</ref> It continually undergoes development by way of numerous physical, chemical and biological processes, which include [[weathering]] with associated [[erosion]].<ref>{{cite book |first=Richard John |last=Huggett |chapter=What is geomorphology? |title=Fundamentals of geomorphology |edition=4th |series=Routledge Fundamentals of Physical Geography |publisher=[[Routledge]] |location=London, United Kingdom |year=2017 |pages=3–30 |isbn=978-1-138-94065-9 |url=https://archive.org/details/routledgefundamentalsofphysical/mode/2up |access-date=12 November 2025 }}</ref> Given its complexity and strong internal [[connectedness]], [[Soil ecology|soil ecologists]] regard soil as an [[ecosystem]].<ref>{{cite journal |last=Ponge |first=Jean-François |date=21 April 2015 |title=The soil as an ecosystem |url=https://www.researchgate.net/publication/276090499 |journal=Biology and Fertility of Soils |volume=51 |issue=6 |pages=645–8 |doi=10.1007/s00374-015-1016-1 |bibcode=2015BioFS..51..645P |access-date=12 November 2025 |s2cid=18251180 }}</ref>

Most soils have a dry [[bulk density]] (density of soil taking into account voids when dry) between 1.1 and 1.6&nbsp;g/cm<sup>3</sup>, though the soil [[Particle density (packed density)|particle density]] is much higher, in the range of 2.6 to 2.7&nbsp;g/cm<sup>3</sup>.<ref>{{cite web |last1=Yu |first1=Charley |last2=Kamboj |first2=Sunita |last3=Wang |first3=Cheng |last4=Cheng |first4=Jing-Jy |year=2015 |title=Data collection handbook to support modeling impacts of radioactive material in soil and building structures |url=https://resrad.evs.anl.gov/docs/data_collection.pdf |url-status=live |archive-url=https://web.archive.org/web/20180804105951/http://resrad.evs.anl.gov/docs/data_collection.pdf |archive-date=4 August 2018 |access-date=12 November 2025 |website=[[Argonne National Laboratory]] |pages=13–21 }}</ref> Little of the soil of [[planet Earth]] is older than the [[Pleistocene]] and none is older than the [[Cenozoic]],<ref name="Buol2011">{{cite book |last1=Buol |first1=Stanley W. |url=https://fr.1lib.sk/book/2156097/71790f |title=Soil genesis and classification |last2=Southard |first2=Randal J. |last3=Graham |first3=Robert C. |last4=McDaniel |first4=Paul A. |date=2011 |publisher=[[Wiley-Blackwell]] |isbn=978-0-470-96060-8 |edition=6th |location=Ames, Iowa |access-date=12 November 2025 }}</ref> although [[Paleopedological record|fossilized soils]] are preserved from as far back as the [[Archean]].<ref>{{cite journal |last1=Retallack |first1=Gregory J. |last2=Krinsley |first2=David H. |last3=Fischer |first3=Robert |last4=Razink |first4=Joshua J. |last5=Langworthy |first5=Kurt A. |date=December 2016 |title=Archean coastal-plain paleosols and life on land |url=https://cpb-us-e1.wpmucdn.com/blogs.uoregon.edu/dist/d/3735/files/2013/07/Retallack-et-al.-2016-Farrel-1gt7uft.pdf |url-status=live |journal=[[Gondwana Research]] |volume=40 |pages=1–20 |bibcode=2016GondR..40....1R |doi=10.1016/j.gr.2016.08.003 |archive-url=https://web.archive.org/web/20181113075710/https://cpb-us-e1.wpmucdn.com/blogs.uoregon.edu/dist/d/3735/files/2013/07/Retallack-et-al.-2016-Farrel-1gt7uft.pdf |archive-date=13 November 2018 |access-date=12 November 2025 }}</ref>

Collectively the Earth's body of soil is called the [[pedosphere]]. The pedosphere interfaces with the [[lithosphere]], the [[hydrosphere]], the [[atmosphere]], and the [[biosphere]].<ref>{{cite book |url=https://fr.1lib.sk/book/28751405/35ce47 |title=Encyclopedia of soil science |year=2008 |publisher=[[Springer Science+Business Media|Springer]] |isbn=978-1-4020-3994-2 |editor-last=Chesworth |editor-first=Ward |edition=1st |location=Dordrecht, The Netherlands |access-date=12 November 2025 |archive-url=https://web.archive.org/web/20180905002957/http://www.encyclopedias.biz/dw/Encyclopedia%20of%20Soil%20Science.pdf |archive-date=5 September 2018 |url-status=live }}</ref> Soil has four important [[soil functions|functions]]:

* as a medium for [[plant growth]]
* as a means of [[water storage]], [[water supply]], and [[water purification]]
* as a modifier of [[Atmosphere of Earth|Earth's atmosphere]]
* as a habitat for [[soil organisms]]

All of these functions, in their turn, modify the soil and its properties.

[[Soil science]] has two basic branches of study: [[edaphology]] and [[pedology]]. ''Edaphology'' studies the influence of soils on living things.<ref>{{cite web |url=https://sis.agr.gc.ca/cansis/glossary/e/index.html |title=Glossary of terms in soil science |website=[[Agriculture and Agri-Food Canada]] |date=7 June 2021 |archive-url=https://web.archive.org/web/20181027045042/http://sis.agr.gc.ca/cansis/glossary/e/index.html |archive-date=27 October 2018 |url-status=live |access-date=12 November 2025 }}</ref> ''Pedology'' focuses on the formation, description (morphology), and classification of soils in their natural environment.<ref>{{cite book |last=Amundson |first=Ronald |title=Introduction to the biogeochemistry of soils |year=2021 |publisher=[[Cambridge University Press]] |isbn=978-1-108-83126-0  |editor-last=Amundson |editor-first=Ronald |edition=1st |location=Cambridge, United Kingdom |pages=1–10 |chapter=Introduction to soils |doi=10.1017/9781108937795 |chapter-url=https://assets.cambridge.org/97811088/31260/excerpt/9781108831260_excerpt.pdf |access-date=12 November 2025 }}</ref> In [[engineering]] terms, soil is included in the broader concept of [[regolith]], which also includes other loose material that lies above the [[bedrock]], as can be found on the [[Moon]] and other [[Astronomical object|celestial objects]].<ref>{{cite web |url=https://www.mps.mpg.de/phd/planetary-interiors-and-surfaces-2011-part-05 |title=Impacts and formation of regolith |last1=Küppers |first1=Michael |last2=Vincent |first2=Jean-Baptiste |website=[[Max Planck Institute for Solar System Research]] |archive-url=https://web.archive.org/web/20180804200824/https://www.mps.mpg.de/phd/planetary-interiors-and-surfaces-2011-part-05 |archive-date=4 August 2018 |url-status=live |access-date=12 November 2025 }}</ref>

== Processes ==

Soil is a major component of the [[Earth]]'s [[ecosystem]]. The world's ecosystems are impacted in far-reaching ways by the processes carried out in the soil, with effects ranging from [[ozone depletion]] and [[global warming]] to [[rainforest destruction]] and [[water pollution]]. With respect to Earth's [[carbon cycle]], soil acts as an important [[carbon sink|carbon reservoir]],<ref>{{cite journal |last1=Amelung |first1=Wulf |last2=Bossio |first2=Deborah |last3=De Vries |first3=Wim |last4=Kögel-Knabner |first4=Ingrid |author4-link=Ingrid Kögel-Knabner |last5=Lehmann |first5=Johannes |last6=Amundson |first6=Ronald |last7=Bol |first7=Roland |last8=Collins |first8=Chris |last9=Lal |first9=Rattan |last10=Leifeld |first10=Jens |last11=Minasny |first11=Buniman |last12=Pan |first12=Gen-Xing |last13=Paustian |first13=Keith |last14=Rumpel |first14=Cornelia |last15=Sanderman |first15=Jonathan |last16=Van Groeningen |first16=Jan Willem |last17=Mooney |first17=Siân |last18=Van Wesemael |first18=Bas |last19=Wander |first19=Michelle |last20=Chabbi |first20=Abad |date=27 October 2020 |title=Towards a global-scale soil climate mitigation strategy |journal=[[Nature Communications]] |language=en |volume=11 |issue=1 |article-number=5427 |doi=10.1038/s41467-020-18887-7 |pmid=33110065 |pmc=7591914 |bibcode=2020NatCo..11.5427A |issn=2041-1723 |doi-access=free }}</ref> and it is potentially one of the most reactive to human disturbance<ref>{{cite journal |last1=Pouyat |first1=Richard |last2=Groffman |first2=Peter |last3=Yesilonis |first3=Ian |last4= Hernandez |first4=Luis |journal=[[Environmental Pollution (journal)|Environmental Pollution]] |volume=116 |issue=Supplement 1 |title=Soil carbon pools and fluxes in urban ecosystems |url=https://www.researchgate.net/publication/11526697 |date=February 2002 |pages=S107–S118 |doi=10.1016/S0269-7491(01)00263-9 |pmid=11833898 |access-date=12 November 2025 |quote=Our analysis of pedon data from several disturbed soil profiles suggests that physical disturbances and anthropogenic inputs of various materials (direct effects) can greatly alter the amount of C stored in these human "made" soils. }}</ref> and [[climate change]].<ref>{{cite journal |last1=Davidson |first1=Eric A. |last2=Janssens |first2=Ivan A. |journal=[[Nature (journal)|Nature]] |volume=440 |title=Temperature sensitivity of soil carbon decomposition and feedbacks to climate change |date=9 March 2006 |issue=7081 |pages=165‒73 |url=https://www.researchgate.net/publication/7253750 |doi=10.1038/nature04514 |pmid=16525463 |bibcode=2006Natur.440..165D |s2cid=4404915 |access-date=12 November 2025 }}</ref> As the planet warms, it has been predicted that soils will add [[carbon dioxide]] to the atmosphere due to increased [[Soil biology|biological]] activity at higher temperatures, a [[positive feedback]] (amplification).<ref>{{cite journal |last=Powlson |first=David |journal=[[Nature (journal)|Nature]] |volume=433 |title=Will soil amplify climate change? |date=19 January 2005 |issue=20 January 2005 |pages=204‒5 |url=https://fr.1lib.sk/book/42664152/aa2c51 |doi=10.1038/433204a |pmid=15662396 |bibcode=2005Natur.433..204P |s2cid=35007042 |access-date=13 November 2025 }}</ref> This prediction has, however, been questioned on consideration of more recent knowledge on [[soil carbon]] turnover.<ref>{{cite journal |last1=Bradford |first1=Mark A. |last2=Wieder |first2=William R. |last3=Bonan |first3=Gordon B. |last4=Fierer |first4=Noah |last5=Raymond |first5=Peter A. |last6=Crowther |first6=Thomas W. |journal=[[Nature Climate Change]] |volume=6 |title=Managing uncertainty in soil carbon feedbacks to climate change |url=https://fr.1lib.sk/book/91686045/7e7aac |date=27 July 2016 |issue=8 |pages=751–8 |doi=10.1038/nclimate3071 |access-date=13 November 2025 |bibcode=2016NatCC...6..751B |s2cid=43955196 |archive-date=10 April 2017 |archive-url=https://web.archive.org/web/20170410025316/http://fiererlab.org/wp-content/uploads/2014/09/Bradford_etal_2016_NCC.pdf |url-status=live }}</ref>

Soil acts as an [[ecological engineering|engineering]] medium, a habitat for [[soil organisms]], a recycling system for [[Nutrient cycle|nutrients]] and [[organic waste]]s, a regulator of [[water quality]], a modifier of [[Atmospheric chemistry|atmospheric composition]], and a medium for [[plant growth]], making it a critically important provider of [[ecosystem services]].<ref>{{cite journal |last1=Dominati |first1=Estelle |last2=Patterson |first2=Murray |last3=Mackay |first3=Alec |journal=[[Ecological Economics (journal)|Ecological Economics]] |volume=69 |issue=9 |title=A framework for classifying and quantifying the natural capital and ecosystem services of soils |date=15 July 2010 |url=https://www.researchgate.net/publication/223852147 |pages=1858‒68 |doi=10.1016/j.ecolecon.2010.05.002 |bibcode=2010EcoEc..69.1858D |access-date=13 November 2025 |archive-url=https://web.archive.org/web/20170808082847/http://esanalysis.colmex.mx/Sorted%20Papers/2010/2010%20NZL%20-3F%20Phys.pdf |archive-date=8 August 2017 |url-status=live }}</ref> Since soil has a tremendous range of available [[Ecological niche|niches]] and [[habitat]]s, it contains a prominent part of the Earth's [[genetic diversity]]. A gram of soil can contain billions of organisms, belonging to thousands of species, mostly microbial and largely still unexplored.<ref>{{cite journal |last=Dykhuizen |first=Daniel E. |journal=[[Antonie van Leeuwenhoek (journal)|Antonie van Leeuwenhoek]] |volume=73 |issue=1 |title=Santa Rosalia revisited: why are there so many species of bacteria? |date=January 1998 |url=https://www.researchgate.net/publication/13682480 |pages=25‒33 |doi=10.1023/A:1000665216662 |pmid=9602276 |s2cid=17779069 |access-date=13 November 2025 }}</ref><ref>{{cite journal |last1=Torsvik |first1=Vigdis |last2=Øvreås |first2=Lise |journal=[[Current Opinion in Microbiology]] |volume=5 |issue=3 |title=Microbial diversity and function in soil: from genes to ecosystems |date=1 June 2002 |pages=240‒5 |url=https://www.academia.edu/13038690 |doi=10.1016/S1369-5274(02)00324-7 |pmid=12057676 |access-date=13 November 2025 }}</ref> Soil has a [[mean]] [[Prokaryote|prokaryotic]] density of roughly 10<sup>8</sup> organisms per gram,<ref>{{cite journal |last1=Raynaud |first1=Xavier |last2=Nunan |first2=Naoise |journal=[[PLOS ONE]] |volume=9 |issue=1 |title=Spatial ecology of bacteria at the microscale in soil |date=28 January 2014 |article-number=e87217 |doi=10.1371/journal.pone.0087217 |pmid=24489873 |pmc=3905020 |bibcode=2014PLoSO...987217R |doi-access=free }}</ref> whereas the ocean has no more than 10<sup>7</sup> prokaryotic organisms per milliliter (gram) of seawater.<ref>{{cite journal |last1=Whitman |first1=William B. |last2=Coleman |first2=David C. |last3=Wiebe |first3=William J. |journal=[[Proceedings of the National Academy of Sciences of the USA]] |volume=95 |issue=12 |title=Prokaryotes: the unseen majority |date=9 June 1998 |pages=6578‒83 |doi=10.1073/pnas.95.12.6578 |pmid=9618454 |pmc=33863 |bibcode=1998PNAS...95.6578W |url=https://www.academia.edu/10294375 |access-date=13 November 2025 }}</ref> [[Soil organic matter|Organic carbon]] held in soil is eventually returned to the atmosphere through the process of [[cellular respiration|respiration]] carried out by [[heterotrophic]] organisms, but a substantial part is retained in the soil in the form of [[soil organic matter]]; [[tillage]] usually increases the rate of [[soil respiration]], leading to the depletion of soil organic matter.<ref>{{cite journal |last1=Schlesinger |first1=William H. |last2=Andrews |first2=Jeffrey A. |journal=Biogeochemistry |volume=48 |issue=1 |title=Soil respiration and the global carbon cycle |date=January 2000 |url=https://www.researchgate.net/publication/51997678 |pages=7‒20 |doi=10.1023/A:1006247623877 |bibcode=2000Biogc..48....7S |s2cid=94252768 |access-date=13 November 2025 }}</ref> Since plant roots need oxygen, [[aeration]] is an important characteristic of soil. This ventilation can be accomplished via networks of interconnected [[Pore space in soil|soil pores]], which also absorb and hold rainwater making it readily available for uptake by plants.<ref>{{cite journal |last1=Arthur |first1=Emmanuel |last2=Moldrup |first2=Per |last3=Schjønning |first3=Per |last4=De Jonge |first4=Lis Wollesen |journal=[[Soil Science Society of America Journal]] |volume=77 |issue=6 |title=Water retention, gas transport, and pore network complexity during short-term regeneration of soil structure |date=November-December 2013 |pages=1965‒76 |doi=10.2136/sssaj2013.07.0270 |url=https://www.researchgate.net/publication/258239096 |access-date=13 November 2025 }}</ref> Since plants require a nearly continuous supply of water, but most regions receive sporadic rainfall, the [[Soil water (retention)|water-holding capacity]] of soils is vital for plant survival.<ref>{{cite journal |last1=Denmead |first1=Owen Thomas |last2=Shaw |first2=Robert Harold |journal=[[Agronomy Journal]] |volume=54 |issue=5 |title=Availability of soil water to plants as affected by soil moisture content and meteorological conditions |date=September-October 1962 |url=https://www.researchgate.net/publication/250098028 |pages=385‒90 |doi=10.2134/agronj1962.00021962005400050005x |bibcode=1962AgrJ...54..385D |access-date=14 November 2025 }}</ref>

Soils can effectively remove impurities,<ref>{{cite journal |last1=House |first1=Christopher H. |last2=Bergmann |first2=Ben A. |last3=Stomp |first3=Anne-Marie |last4=Frederick |first4=Douglas J. |journal=Ecological Engineering |volume=12 |issue=1–2 |title=Combining constructed wetlands and aquatic and soil filters for reclamation and reuse of water |date=January 1999 |url=https://fr.1lib.sk/book/36395340/5a259d |pages=27–38 |doi=10.1016/S0925-8574(98)00052-4 |bibcode=1999EcEng..12...27H |access-date=14 November 2025 }}</ref> kill disease agents,<ref>{{cite journal |last1=Van Bruggen |first1=Ariena H.C. |last2=Semenov |first2=Alexander M. |journal=Applied Soil Ecology |volume=15 |issue=1 |title=In search of biological indicators for soil health and disease suppression |date=August 2000 |url=https://www.researchgate.net/publication/222520930 |pages=13–24 |doi=10.1016/S0929-1393(00)00068-8 |bibcode=2000AppSE..15...13V |access-date=14 November 2025 }}</ref> and degrade [[contaminants]], this latter property being called [[natural attenuation]].<ref>{{cite web |url=https://semspub.epa.gov/work/HQ/401611.pdf |title=Community guide to monitored natural attenuation |access-date=14 November 2025 }}</ref> Typically, soils maintain a net absorption of [[oxygen]] and [[methane]] and undergo a net release of [[carbon dioxide]] and [[nitrous oxide]].<ref>{{cite journal |last1=Linn |first1=Daniel Myron |last2=Doran |first2=John W. |journal=[[Soil Science Society of America Journal]] |volume=48 |issue=6 |title=Effect of water-filled pore space on carbon dioxide and nitrous oxide production in tilled and nontilled soils |date=November–December 1984 |url=https://fr.1lib.sk/book/55339558/7bc22a |pages=1267–72 |doi=10.2136/sssaj1984.03615995004800060013x |access-date=14 November 2025 |bibcode=1984SSASJ..48.1267L }}</ref> Soils offer plants physical support, air, water, temperature moderation, nutrients, and protection from toxins.<ref>{{cite book |last1=Gregory |first1=Peter J. |last2=Nortcliff |first2=Stephen |date=2013 |title=Soil conditions and plant growth |isbn=978-1-4051-9770-0 |publisher=[[Wiley-Blackwell]] |location=Hoboken, New Jersey |url=https://fr.1lib.sk/book/2156095/a3577f |access-date=14 November 2025 }}</ref> Soils provide readily available nutrients to plants and animals by converting dead organic matter into various nutrient forms.<ref>{{cite book |last1=Bot |first1=Alexandra |last2=Benites |first2=José |date=2005 |title=The importance of soil organic matter: key to drought-resistant soil and sustained food and production |isbn=978-92-5-105366-9 |publisher=[[Food and Agriculture Organization of the United Nations]] |location=Rome, Italy |url=http://www.fao.org/3/a-a0100e.pdf |access-date=14 November 2025 }}</ref>

== Composition ==
[[File:Estructura-suelo.jpg|thumb|alt= This is a diagram and related photograph of soil layers from bedrock to soil.|A, B, and C represent the [[soil horizon|soil profile]], a notation firstly coined by [[Vasily Dokuchaev]] (1846–1903), the father of pedology. Here, A is the [[topsoil]]; B is a [[regolith]]; C is a [[saprolite]] (a less-weathered regolith); the bottom-most layer represents the [[bedrock]].]]
{{Pie chart
|caption = Components of a silt loam soil by percent volume
|value1 = 25
|label1 = Water
|color1 = blue
|value2 = 25
|label2 = Gases
|color2 = cyan
|value3 = 18
|label3 = Sand
|color3 = yellow
|value4 = 18
|label4 = Silt
|color4 = brown
|value5 = 9
|label5 = Clay
|color5 = grey
|value6 = 5
|label6 = Organic matter
|color6 = black
}}

A typical soil is about 50% solids (45% mineral and 5% organic matter), and 50% voids (or pores) of which half is occupied by water and half by gas.<ref>{{cite web |last=McClellan |first=Tai |title=Soil composition |url=https://www.ctahr.hawaii.edu/mauisoil/a_comp.aspx |publisher=[[University of Hawaiʻi]] at Mānoa, College of Tropical Agriculture and Human Resources |access-date=14 November 2025 }}</ref> The percent soil mineral and organic content can be treated as a constant (in the short term), while the percent soil water and gas content is considered highly variable whereby a rise in one is simultaneously balanced by a reduction in the other.<ref>{{cite book |last=Zhang |first=Hailin |title=Master Gardener's Manual |url=https://extension.okstate.edu/fact-sheets/print-publications/e/master-gardeners-handbook-e-1034.pdf |pages=54–63 |publisher=Oklahoma Cooperative Extension, Service Division of Agricultural Sciences and Natural Resources, [[Oklahoma State University]] |location=Stillwater, Oklahoma |access-date=14 November 2025 }}</ref> The [[pore space]] allows for the infiltration and movement of air and water, both of which are critical for life existing in soil.<ref name="Vannier1987">{{cite journal |last=Vannier |first=Guy |journal=Biology and Fertility of Soils |volume=3 |issue=1 |title=The porosphere as an ecological medium emphasized in Professor Ghilarov's work on soil animal adaptations |date=February 1987 |url=https://fr.1lib.sk/book/37554227/660688 |pages=39–44 |doi=10.1007/BF00260577 |bibcode=1987BioFS...3...39V |s2cid=297400 |access-date=14 November 2025 }}</ref> [[Soil compaction|Compaction]], a common problem with soils, in particular under heavy machinery traffic,<ref>{{cite journal |last1=Shaheb |first1=Md Rayhan |last2=Venkatesh |first2=Ramarao |last3=Shearer |first3=Scott A. |journal=Journal of Biosystems Engineering |volume=46 |issue=3 |title=A Review on the effect of soil compaction and its management for sustainable crop production |date=24 November 2021 |pages=417‒39 |doi=10.1007/s42853-021-00117-7 |url=https://www.researchgate.net/publication/356506449 |access-date=13 November 2025 }}</ref> reduces this space, preventing air and water from reaching plant roots and soil organisms.<ref>{{cite journal |last1=Torbert |first1=H. Allen |last2=Wood |first2=Wes |journal=Communications in Soil Science and Plant Analysis |volume=23 |issue=11 |title=Effect of soil compaction and water-filled pore space on soil microbial activity and N losses |year=1992 |url=https://www.researchgate.net/publication/240546132 |pages=1321‒31 |doi=10.1080/00103629209368668 |bibcode=1992CSSPA..23.1321T |access-date=14 November 2025 }}</ref>

Given sufficient time, an undifferentiated soil will evolve a [[soil horizon|soil profile]] that consists of two or more layers, referred to as [[soil horizon]]s. These differ in one or more properties such as in their [[Soil texture|texture]], [[structure]], [[density]], [[porosity]], [[Viscosity|consistency]], temperature, color, and [[Reactivity (chemistry)|reactivity]].<ref name="Buol2011"/> The horizons differ greatly in thickness and generally lack sharp boundaries; their development is dependent on the type of [[parent material]], the processes that modify those parent materials (e.g. [[mineral weathering]]), and the [[Soil formation#Factors|soil-forming factors]] that influence those processes. The biological influences on soil properties (e.g. [[bioturbation]]) are strongest near the surface, while the [[geochemical]] influences on soil properties increase with depth. Mature soil profiles typically include three basic master horizons: A, B, and C. The [[solum]] normally includes the A and B horizons. The living component of the soil is largely confined to the solum, and is generally more prominent in the A horizon.{{sfn|Simonson|1957|p=17}} It has been suggested that the ''pedon'', a column of soil extending vertically from the surface to the underlying [[parent material]] and large enough to show the characteristics of all its horizons, could be subdivided in the ''humipedon'' (the living part, where most soil organisms are dwelling, corresponding to the ''[[humus form]]''), the ''copedon'' (in intermediary position, where most [[weathering]] of minerals takes place) and the ''lithopedon'' (in contact with the subsoil).<ref>{{cite journal |last1=Zanella |first1=Augusto |last2=Katzensteiner |first2=Klaus |last3=Ponge |first3=Jean-François |last4=Jabiol |first4=Bernard |last5=Sartori |first5=Giacomo |last6=Kolb |first6=Eckart |last7=Le Bayon |first7=Renée-Claire |last8=Aubert |first8=Michaël |last9=Ascher-Jenull |first9=Judith |last10=Englisch |first10=Michael |last11=Hager |first11=Herbert |title=TerrHum: an iOS App for classifying terrestrial humipedons and some considerations about soil classification |journal=[[Soil Science Society of America Journal]] |date=June 2019 |volume=83 |issue=S1 |pages=S42–S48 |doi=10.2136/sssaj2018.07.0279 |s2cid=197555747 |url=https://www.researchgate.net/publication/332080061 |access-date=14 November 2025 }}</ref>

The soil [[Texture (geology)|texture]] is determined by the relative proportions of the individual particles of [[sand]], [[silt]], and [[clay]] that make up the soil. [[File:SoilTextureTriangle.svg|thumb|A [[Soil triangle|soil texture triangle]] plot is a visual representation of the proportions of sand, silt, and clay in a soil sample.]] The interaction of the individual mineral particles with organic matter, water, gases via [[Biotic component|biotic]] and [[abiotic]] processes causes those particles to [[flocculate]] (stick together) to form [[soil structure|aggregates]] or [[ped]]s.<ref>{{cite journal |last1=Bronick |first1=Carol J. |last2=Lal |first2=Ratan |title=Soil structure and management: a review |journal=Geoderma |date=January 2005 |volume=124 |issue=1–2 |pages=3–22 |doi=10.1016/j.geoderma.2004.03.005 |url=https://www.academia.edu/72307009 |access-date=14 November 2025 |bibcode=2005Geode.124....3B }}</ref> Where these aggregates can be identified, a soil can be said to be developed, and can be described further in terms of color, porosity, consistency, reaction ([[acidity]]), etc.

Water is a critical agent in soil development due to its involvement in the dissolution, precipitation, erosion, transport, and deposition of the materials of which a soil is composed.<ref>{{cite web |url=https://www.fao.org/3/r4082e/r4082e03.htm |title=Soil and water |website=[[Food and Agriculture Organization of the United Nations]] |access-date=14 November 2025 }}</ref> The mixture of water and dissolved or suspended materials that occupy the soil [[pore space]] is called the ''soil solution''. Since [[Soil water (retention)|soil water]] is never pure water, but contains hundreds of dissolved organic and mineral substances, it may be more accurately called the ''soil solution''. Water is central to the [[Dissolution (chemistry)|dissolution]], [[Precipitation (chemistry)|precipitation]] and [[Leaching (agriculture)|leaching]] of minerals from the [[soil profile]]. Finally, water affects the type of vegetation that grows in a soil, which in turn affects the development of the soil, a complex feedback which is exemplified in the dynamics of banded vegetation patterns in semi-arid regions.<ref>{{cite journal |last1=Valentin |first1=Christian |last2=d'Herbès |first2=Jean-Marc |last3=Poesen |first3=Jean |journal=Catena |volume=37 |issue=1 |title=Soil and water components of banded vegetation patterns |date=September 1999 |url=https://www.academia.edu/35300713 |pages=1‒24 |doi=10.1016/S0341-8162(99)00053-3 |bibcode=1999Caten..37....1V |access-date=14 November 2025 }}</ref>

Soils supply [[plant]]s with [[nutrient]]s, most of which are held in place by particles of [[Soil texture#Soil separates|clay]] and organic matter ([[colloid]]s)<ref>{{cite book |last1=Brady |first1=Nyle C. |last2=Weil |first2=Ray R. |year=2007 |chapter=The colloidal fraction: seat of soil chemical and physical activity |title=The nature and properties of soils |pages=310–57 |edition=14th |editor-last1=Brady |editor-first1=Nyle C. |editor-last2=Weil |editor-first2=Ray R. |publisher=[[Pearson Education|Pearson]] |location=London, United Kingdom |isbn=978-0-13-227938-3 |chapter-url=https://www.researchgate.net/publication/309630422 |access-date=14 November 2025 }}</ref> The nutrients may be [[Adsorption|adsorbed]] on [[clay mineral]] surfaces, bound within clay minerals ([[Absorption (chemistry)|absorbed]]), or bound within organic compounds as part of the living [[Soil organism|organisms]] or dead soil organic matter (humus).<ref name="Ponge2022"/> These bound nutrients interact with soil water to [[Buffer solution|buffer]] the soil solution composition (attenuate changes in the soil solution) as soils wet up or dry out, as plants take up nutrients, as salts are leached, or as acids or alkalis are added.<ref>{{cite web |url=http://eagri.org/eagri50/SSAC121/lec14.pdf |title=Soil colloids: properties, nature, types and significance |website=[[Tamil Nadu Agricultural University]] |access-date=14 November 2025 }}</ref>

Plant [[Plant nutrients in soil|nutrient availability]] is affected by [[soil pH]], which is a measure of the [[hydrogen]] [[Thermodynamic activity|ion activity]] in the soil solution. Soil pH is a function of many soil forming factors, and is generally lower (more acidic) where [[weathering]] is more advanced.<ref>{{cite web |url=https://www.researchgate.net/publication/305775103 |last=Miller |first=Jarrod Ottis |title=Soil pH affects nutrient availability |access-date=14 November 2025 }}</ref>

Most plant nutrients, with the exception of [[nitrogen]], [[nitrogen fixation|fixed]] from the atmosphere, originate from the minerals that make up the soil [[parent material]]. Some nitrogen also originates from rain as dilute [[nitric acid]] and [[ammonia]],<ref>{{cite journal |last1=Goulding |first1=Keith W. T. |last2=Bailey |first2=Neal J. |last3=Bradbury |first3=Nicola J. |last4=Hargreaves |first4=Patrick |last5=Howe |first5=M. T. |last6=Murphy |first6=Daniel V. |last7=Poulton |first7=Paul R. |last8=Willison |first8=Toby W. |journal=[[New Phytologist]] |volume=139 |issue=1 |title=Nitrogen deposition and its contribution to nitrogen cycling and associated soil processes |date=May 1998 |pages=49‒58 |doi=10.1046/j.1469-8137.1998.00182.x |doi-access=free |bibcode=1998NewPh.139...49G }}</ref> but most of the nitrogen is available in soils as a result of [[nitrogen fixation]] by [[diazotroph]] [[bacteria]] (e.g. [[cyanobacteria]] with [[Heterocyst|heterocysts]], [[Clostridium]]). Once in the soil-plant system, most nutrients are recycled through living organisms, plant and microbial residues ([[soil organic matter]]), mineral-bound forms ([[humus]]), and the soil solution. Both living soil organisms (microbes, animals and plant roots) and soil organic matter are of critical importance to this recycling, and thereby to [[soil formation]] and [[soil fertility]].<ref>{{cite book |last=Kononova |first=M. M. |year=1966 |title=Soil organic matter: its nature, its role in soil formation and in soil fertility |edition=2nd |publisher=[[Elsevier]] |location=Amsterdam, the Netherlands |isbn=978-1-4831-8568-2 |url=https://fr.1lib.sk/book/2275488/56c210 |access-date=14 November 2025 }}</ref> Microbial [[soil enzyme|enzymes]] may release nutrients from minerals or organic matter for use by plants and other microorganisms, sequester (incorporate) them into living cells, or cause their loss from the soil by [[volatilisation]] (loss to the atmosphere as gases) or leaching.<ref>{{cite journal |last1=Burns |first1=Richards G. |last2=DeForest |first2=Jared L. |last3=Marxsen |first3=Jürgen |last4=Sinsabaugh |first4=Robert L. |last5=Stromberger |first5=Mary E. |last6=Wallenstein |first6=Matthew D. |last7=Weintraub |first7=Michael N. |last8=Zoppini |first8=Annamaria |journal=[[Soil Biology and Biochemistry]] |volume=58 |title=Soil enzymes in a changing environment: current knowledge and future directions |date=March 2013 |pages=216‒34 |doi=10.1016/j.soilbio.2012.11.009 |bibcode=2013SBiBi..58..216B |url=https://www.academia.edu/25235991 |access-date=14 November 2025 }}</ref>

== Formation ==
{{main|Soil formation}}
{{Further|Soil mechanics#Genesis}}
Soil is said to be formed when organic matter has accumulated and colloids are washed downward, leaving deposits of [[Clay mineral|clay]], [[humus]], [[iron oxide]], [[carbonate]], and [[gypsum]], producing a distinct layer called the B [[Soil horizon|horizon]]. This is a somewhat arbitrary definition as mixtures of [[sand]], [[silt]], clay and humus will support biological and agricultural activity before that time.<ref>{{cite journal |last1=Sengupta |first1=Aditi |last2=Kushwaha |first2=Priyanka |last3=Jim |first3=Antonia |last4=Troch |first4=Peter A. |last5=Maier |first5=Raina |date=21 May 2020 |title=New soil, old plants, and ubiquitous microbes: evaluating the potential of incipient basaltic soil to support native plant growth and influence belowground soil microbial community composition |journal=[[Sustainability (journal)|Sustainability]] |volume=12 |issue=10 |article-number=4209 |doi=10.3390/su12104209 |doi-access=free |bibcode=2020Sust...12.4209S |hdl=10150/649287 |hdl-access=free }}</ref> These constituents are moved from one level to another by water ([[Leaching (agriculture)|leaching]]) and animal activity ([[bioturbation]]). As a result, layers (horizons) form in the soil profile. The alteration ([[weathering]]) and movement of materials within a soil causes the formation of distinctive [[soil horizons]]. However, more recent definitions of soil embrace soils without any organic matter, such as those [[regolith]]s that formed on Mars<ref>{{cite journal |last1=Bishop |first1=Janice L. |last2=Murchie |first2=Scott L. |last3=Pieters |first3=Carlé L. |last4=Zent |first4=Aaron P. |date=6 November 2002 |title=A model for formation of dust, soil, and rock coatings on Mars: physical and chemical processes on the Martian surface |journal=[[Journal of Geophysical Research]] |volume=107 |issue=E11 |pages=7-1–7-17 |doi=10.1029/2001JE001581 |bibcode=2002JGRE..107.5097B |doi-access=free }}</ref> and analogous conditions in planet [[Earth]] deserts.<ref>{{cite journal |last1=Navarro-González |first1=Rafael |last2=Rainey |first2=Fred A. |last3=Molina |first3=Paola |last4=Bagaley |first4=Danielle R. |last5=Hollen |first5=Becky J. |last6=de la Rosa |first6=José |last7=Small |first7=Alanna M. |last8=Quinn |first8=Richard C. |last9=Grunthaner |first9=Frank J. |last10=Cáceres |first10=Luis |last11=Gomez-Silva |first11=Benito |last12=McKay |first12=Christopher P. |date=7 November 2003 |title=Mars-like soils in the Atacama desert, Chile, and the dry limit of microbial life |journal=[[Science (journal)|Science]] |volume=302 |issue=5647 |pages=1018–21 |doi=10.1126/science.1089143 |pmid=14605363 |url=https://www.researchgate.net/publication/9020258 |access-date=17 November 2025 |bibcode=2003Sci...302.1018N |s2cid=18220447 }}</ref>

An example of the development of a soil would begin with the [[weathering]] of lava flow [[bedrock]], which would produce the purely mineral-based parent material from which the [[soil texture]] forms. Soil development would proceed most rapidly from bare rock of recent flows in a warm climate, under heavy and frequent rainfall. Under such conditions, plants (in a first stage [[nitrogen-fixing]] [[lichen]]s and [[cyanobacteria]] then [[epilithic]] [[higher plants]]) become established very quickly on [[basalt]]ic lava, even though there is very little organic material.<ref>{{cite journal |last1=Guo |first1=Yong |last2=Fujimura |first2=Reiko |last3=Sato |first3=Yoshinori |last4=Suda |first4=Wataru |last5=Kim |first5=Seok-won |last6=Oshima |first6=Kenshiro |last7=Hattori |first7=Masahira |last8=Kamijo |first8=Takashi |last9=Narisawa |first9=Kazuhiko |last10=Ohta |first10=Hiroyuki |year=2014 |title=Characterization of early microbial communities on volcanic deposits along a vegetation gradient on the island of Miyake, Japan |journal=Microbes and Environments |volume=29 |issue=1 |pages=38–49 |doi=10.1264/jsme2.ME13142 |pmid=24463576 |pmc=4041228 |doi-access=free }}</ref> Basaltic minerals commonly weather relatively quickly, according to the [[Goldich dissolution series]].<ref>{{cite journal |last=Goldich |first=Samuel S. |date=January–February 1938 |title=A study in rock-weathering |url=https://fr.1lib.sk/book/91942187/414bb2 |journal=[[The Journal of Geology]] |volume=46 |issue=1 |pages=17–58 |bibcode=1938JG.....46...17G |doi=10.1086/624619 |issn=0022-1376 |access-date=17 November 2025 |s2cid=128498195 }}</ref> The plants are supported by the porous rock as it is filled with nutrient-bearing water that carries minerals dissolved from the rocks. Crevasses and pockets, local topography of the rocks, would hold fine materials and harbour plant roots. The developing plant roots are associated with mineral-weathering [[Mycorrhiza|mycorrhizal fungi]]<ref>{{cite journal |last1=Van Schöll |first1=Laura |last2=Smits |first2=Mark M. |last3=Hoffland |first3=Ellis |date=22 June 2006 |title=Ectomycorrhizal weathering of the soil minerals muscovite and hornblende |journal=[[New Phytologist]] |volume=171 |issue=4 |pages=805–14 |doi=10.1111/j.1469-8137.2006.01790.x |pmid=16918551 |doi-access=free |bibcode=2006NewPh.171..805V }}</ref> that assist in breaking up the porous lava, and by these means organic matter and a finer mineral soil accumulate with time. Such initial stages of soil development have been described on volcanoes,<ref>{{cite journal |last1=Stretch |first1=Rachelle C. |last2=Viles |first2=Heather A. |date=1 September 2002 |title=The nature and rate of weathering by lichens on lava flows on Lanzarote |journal=[[Geomorphology (journal)|Geomorphology]] |volume=47 |issue=1 |pages=87–94 |doi=10.1016/S0169-555X(02)00143-5 |bibcode=2002Geomo..47...87S |url=https://fr.1lib.sk/book/50018654/f73474 |access-date=17 November 2025 }}</ref> inselbergs,<ref>{{cite journal |last1=Dojani |first1=Stephanie |last2=Lakatos |first2=Michael |last3=Rascher |first3=Uwe |last4=Waneck |first4=Wolfgang |last5=Luettge |first5=Ulrich |last6=Büdel |first6=Burkhard |date=28 September 2007 |title=Nitrogen input by cyanobacterial biofilms of an inselberg into a tropical rainforest in French Guiana |journal=Flora |volume=202 |issue=7 |pages=521–9 |doi=10.1016/j.flora.2006.12.001 |bibcode=2007FMDFE.202..521D |url=https://www.researchgate.net/publication/224026482 |access-date=17 November 2025 }}</ref> and glacial moraines.<ref>{{cite journal |last1=Kabala |first1=Cesary |last2=Kubicz |first2=Justyna |date=April 2012 |title=Initial soil development and carbon accumulation on moraines of the rapidly retreating Werenskiold Glacier, SW Spitsbergen, Svalbard archipelago |journal=Geoderma |volume=175–176 |pages=9–20 |url=https://www.academia.edu/31221217 |doi=10.1016/j.geoderma.2012.01.025 |access-date=17 November 2025 |bibcode=2012Geode.175....9K }}</ref>

How soil formation proceeds is influenced by at least five classic soil-forming factors that are intertwined in the evolution of a soil: [[parent material]], [[climate]], [[topography]] ([[Terrain|relief]]), [[Soil biology|organisms]], and [[time]].<ref>{{cite book |last=Jenny |first=Hans |title=Factors of soil formation: a system of qunatitative pedology |year=1941 |publisher=[[McGraw-Hill]] |location=New York, New York |url=https://netedu.xauat.edu.cn/sykc/hjx/content/ckzl/6/2.pdf |access-date=17 November 2025 |archive-url=https://web.archive.org/web/20170808104008/http://netedu.xauat.edu.cn/sykc/hjx/content/ckzl/6/2.pdf |archive-date=8 August 2017 |url-status=live }}</ref> When reordered to climate, relief, organisms, parent material, and time, they form the acronym CROPT.<ref>{{cite web |url=https://geo.libretexts.org/Bookshelves/Geography_(Physical)/The_Physical_Environment_(Ritter)/11%3A_Soil_Systems/11.05%3A_Factors_Affecting_Soil_Development |title=Factors affecting soil development |first=Michael E. |last=Ritter |date=4 July 2021 |access-date=17 November 2025 }}</ref>

== Physical properties ==
{{main|Physical properties of soil}}
{{for|the academic discipline|Soil physics}}

The physical properties of soils, in order of decreasing importance for [[Ecosystem service|ecosystem services]] such as [[crop production]], are [[Soil texture|texture]], [[Soil structure|structure]], [[bulk density]], [[Pore space in soil|porosity]], consistency, [[temperature]], [[Soil color|colour]] and [[resistivity]].<ref>{{cite book |last1=Gardner |first1=Catriona M.K. |last2=Laryea |first2=Kofi Buna |last3=Unger |first3=Paul W. |year=1999 |title=Soil physical constraints to plant growth and crop production |edition=first |location=Rome, Italy |publisher=[[Food and Agriculture Organization of the United Nations]] |url=https://citeseerx.ist.psu.edu/document?repid=rep1&type=pdf&doi=8dc3f09583443adcb37d380bde37398f479386ba |archive-url=https://web.archive.org/web/20170808175354/http://www.plantstress.com/Files/Soil_Physical_Constraints.pdf |archive-date=8 August 2017 |url-status=live |access-date=17 November 2025 }}</ref> Soil texture is determined by the relative proportion of the three kinds of soil mineral particles, called soil separates: [[sand]], [[silt]], and [[Clay mineral|clay]]. At the next larger scale, soil structures called [[ped]]s or more commonly ''soil aggregates'' are created from the soil separates when [[iron oxide]]s, [[carbonate]]s, clay, [[silica]] and [[humus]], coat particles and cause them to adhere into larger, relatively [[Soil aggregate stability|stable]] secondary structures.<ref>{{cite journal |last1=Six |first1=Johan |last2=Paustian |first2=Keith |last3=Elliott |first3=Edward T. |last4=Combrink |first4=Clay |journal=[[Soil Science Society of America Journal]] |volume=64 |issue=2 |title=Soil structure and organic matter. I. Distribution of aggregate-size classes and aggregate-associated carbon |url=https://www.researchgate.net/publication/280798601 |date=1 March 2000 |pages=681–9 |doi=10.2136/sssaj2000.642681x |access-date=17 November 2025 |bibcode=2000SSASJ..64..681S }}</ref> Soil [[bulk density]], when determined at standardized [[moisture]] conditions, is an estimate of [[Soil compaction (agriculture)|soil compaction]].<ref>{{cite journal |last1=Håkansson |first1=Inge |last2=Lipiec |first2=Jerzy |journal=Soil and Tillage Research |volume=53 |issue=2 |title=A review of the usefulness of relative bulk density values in studies of soil structure and compaction |url=https://www.researchgate.net/publication/222541793 |date=January 2000 |pages=71–85 |doi=10.1016/S0167-1987(99)00095-1 |bibcode=2000STilR..53...71H |s2cid=30045538 |access-date=17 November 2025 |archive-date=16 May 2022 |archive-url=https://web.archive.org/web/20220516120555/http://directory.umm.ac.id/Data%20Elmu/jurnal/S/Soil%20%26%20Tillage%20Research/Vol53.Issue2.Jan2000/1452.pdf |url-status=live }}</ref> Soil [[Pore space in soil|porosity]] consists of the void part of the soil volume and is occupied by gases or water. Soil consistency is the ability of soil materials to stick together. Soil temperature and colour are self-defining. [[Resistivity]] refers to the resistance to conduction of [[electric current]]s and affects the rate of [[corrosion]] of [[metal]] and [[concrete]] structures which are buried in soil.<ref>{{cite journal |last=Schwerdtfeger |first=William J. |journal=[[Journal of Research of the National Bureau of Standards]] |volume=69C |issue=1 |title=Soil resistivity as related to underground corrosion and cathodic protection |date=January–March 1965 |pages=71–7 |doi=10.6028/jres.069c.012 |url=https://nvlpubs.nist.gov/nistpubs/jres/69C/jresv69Cn1p71_A1b.pdf |access-date=17 November 2025 }}</ref> These properties vary through the depth of a soil profile, i.e. through [[soil horizon]]s. Most of these properties determine the [[Permeability of soils|aeration]] of the soil and the ability of water to [[Infiltration (hydrology)|infiltrate]] and to be [[Soil water (retention)|held]] within the soil.<ref>{{cite book |last=Tamboli |first=Prabhakar Mahadeo |year=1961 |title=The influence of bulk density and aggregate size on soil moisture retention |location=Ames, Iowa |publisher=[[Iowa State University]] |url=https://dr.lib.iastate.edu/server/api/core/bitstreams/85621186-4b03-4140-ad1c-b18c3ab3b4a8/content |access-date=17 November 2025 }}</ref>

== Soil moisture ==
{{Main|Soil moisture}}
Soil [[water content]] can be measured as volume or [[Specific weight#Soil mechanics|weight]]. Soil moisture levels, in order of decreasing water content, are [[Water content|saturation]], [[field capacity]], [[wilting point]], air dry, and oven dry. [[Field capacity]] describes a drained wet soil at the point water content reaches equilibrium with gravity. Irrigating soil above field capacity risks [[percolation]] losses. [[Wilting point]] describes the dry limit for growing plants. During growing season, soil moisture is unaffected by plant [[Functional group (ecology)|functional group]]s or [[species richness]] while it varies with [[species composition]].<ref name="Spehn2000">{{cite journal |last1=Spehn |first1=Eva M. |last2=Joshi |first2=Jasmin |last3=Schmid |first3=Bernhard |last4=Alphei |first4=Jörn |last5=Körner |first5=Christian |date=September 2000 |title=Plant diversity effects on soil heterotrophic activity in experimental grassland ecosystems |url=https://www.academia.edu/24032411 |journal=[[Plant and Soil]] |volume=224 |issue=2 |pages=217–30 |doi=10.1023/A:1004891807664 |bibcode=2000PlSoi.224..217S |s2cid=25639544 |access-date=17 November 2025 }}</ref>

[[Available water capacity]] is the amount of water held in a soil profile available to plants. As water content drops, plants have to work against increasing forces of [[adhesion]] and [[sorptivity]] to withdraw water. [[Irrigation scheduling]] avoids [[moisture stress]] by replenishing depleted water before [[Stress (biology)|stress]] is induced.<ref>{{cite web |title=Water holding capacity |work=[[Oregon State University]] |date=24 June 2016 |url=https://forages.oregonstate.edu/ssis/soils/characteristics/water-holding-capacity |quote=Irrigators must have knowledge of the readily available moisture capacity so that water can be applied before plants have to expend excessive energy to extract moisture |access-date=17 November 2025 }}</ref><ref>{{cite web |title=Basics of irrigation scheduling |work=[[University of Minnesota Extension]] |url=https://extension.umn.edu/irrigation/basics-irrigation-scheduling |quote=Only a portion of the available water holding capacity is easily used by the crop before crop water stress develop |access-date=17 November 2025 }}</ref>

[[Capillary action]] is responsible for moving [[groundwater]] from wet regions of the soil to dry areas. [[Subirrigation]] designs (e.g., [[wicking bed]]s, [[sub-irrigated planter]]s) rely on [[Capillary action|capillarity]] to supply water to plant roots. Capillary action can result in an evaporative concentration of salts, causing [[land degradation]] through [[Soil salinity#Dry land salinity|salination]].<ref>{{cite journal |last1=Guo |first1=G. |last2=Araya |first2=K. |last3=Jia |first3=Hongkun |last4=Zhang |first4=Zhigen |last5=Ohomiya |first5=K. |last6=Matsuda |first6=J. |date=May 2006 |title=Improvement of salt-affected soils. I. Interception of capillarity |journal=Biosystems Engineering |volume=94 |issue=1 |pages=139–50 |doi=10.1016/j.biosystemseng.2006.01.012 |url=https://www.academia.edu/18115065 |access-date=17 November 2025 }}</ref>

[[Soil moisture measurement]]—measuring the water content of the soil, as can be expressed in terms of volume or weight—can be based on ''in situ'' probes (e.g., [[capacitance probe]]s, [[neutron probe]]s), or [[remote sensing]] methods. Soil moisture measurement is an important factor in determining changes in soil biological activity.<ref name="Spehn2000"/>

== Soil gas ==
{{main|Soil gas}}
The atmosphere of soil, or [[soil gas]], is very different from the [[Atmosphere of Earth|atmosphere]] above. The consumption of [[oxygen]] by microbes and plant roots, and their release of [[carbon dioxide]], decreases oxygen and increases carbon dioxide concentration. Atmospheric CO<sub>2</sub> concentration is 0.04%, but in the soil pore space it may range from 10 to 100 times that level, thus potentially contributing to the inhibition of root respiration.<ref>{{cite journal |last1=Qi |first1=Jingen |last2=Marshall |first2=John D. |last3=Mattson |first3=Kim G. |journal=[[New Phytologist]] |volume=128 |issue=3 |title=High soil carbon dioxide concentrations inhibit root respiration of Douglas fir |date=November 1994 |pages=435–42 |doi=10.1111/j.1469-8137.1994.tb02989.x |pmid=33874575 |doi-access=free |bibcode=1994NewPh.128..435Q }}</ref> [[Calcareous]] soils regulate CO<sub>2</sub> concentration by [[carbonate]] [[Buffering agent|buffering]], contrary to acid soils in which all CO<sub>2</sub> respired accumulates in the soil pore system.<ref>{{cite journal |last1=Karberg |first1=Noah J. |last2=Pregitzer |first2=Kurt S. |last3=King |first3=John S. |last4=Friend |first4=Aaron L. |last5=Wood |first5=James R. |journal=[[Oecologia]] |volume=142 |issue=2 |title=Soil carbon dioxide partial pressure and dissolved inorganic carbonate chemistry under elevated carbon dioxide and ozone |url=https://www.researchgate.net/publication/8337234 |date=16 September 2004 |pages=296–306 |doi=10.1007/s00442-004-1665-5 |pmid=15378342 |access-date=17 November 2025 |bibcode=2005Oecol.142..296K |s2cid=6161016 }}</ref> At extreme levels, CO<sub>2</sub> is toxic.<ref>{{cite journal |last1=Chang |first1=H. T. |last2=Loomis |first2=Walter E. |journal=[[Plant Physiology (journal)|Plant Physiology]] |volume=20 |issue=2 |title=Effect of carbon dioxide on absorption of water and nutrients by roots |date=1 April 1945 |pages=221–32 |doi=10.1104/pp.20.2.221 |pmid=16653979 |pmc=437214 |doi-access=free }}</ref> This suggests a possible [[negative feedback]] control of soil CO<sub>2</sub> concentration through its inhibitory effects on root and microbial respiration (also called [[soil respiration]]).<ref>{{cite journal |last1=McDowell |first1=Nate J. |last2=Marshall |first2=John D. |last3=Qi |first3=Jingen |last4=Mattson |first4=Kim |journal=Tree Physiology |volume=19 |issue=9 |title=Direct inhibition of maintenance respiration in western hemlock roots exposed to ambient soil carbon dioxide concentrations |date=July 1999 |pages=599–605 |doi=10.1093/treephys/19.9.599 |pmid=12651534 |url=https://www.researchgate.net/publication/10842414 |access-date=17 November 2025 }}</ref> In addition, the soil voids are saturated with [[Water vapor|water vapour]], at least until the point of maximal [[hygroscopic]]ity, beyond which a [[vapour-pressure deficit]] occurs in the soil pore space.<ref name="Vannier1987"/> Adequate porosity is necessary, not just to allow the penetration of water, but also to allow gases to diffuse in and out. Movement of gases is by [[diffusion]] from high concentrations to lower, the [[diffusion coefficient]] decreasing with [[Soil compaction (agriculture)|soil compaction]].<ref>{{cite journal |last1=Xu |first1=Xia |last2=Nieber |first2=John L. |last3=Gupta |first3=Satish C. |journal=[[Soil Science Society of America Journal]] |volume=56 |issue=6 |title=Compaction effect on the gas diffusion coefficient in soils |url=https://www.academia.edu/6547475 |date=November–December 1992 |pages=1743–50 |doi=10.2136/sssaj1992.03615995005600060014x |access-date=17 November 2025 |bibcode=1992SSASJ..56.1743X }}</ref> Oxygen from above atmosphere diffuses in the soil where it is consumed and levels of carbon dioxide in excess of above atmosphere diffuse out with other gases (including [[greenhouse gases]]) as well as [[water vapor]].<ref name="Smith2003">{{cite journal |last1=Smith |first1=Keith A. |last2=Ball |first2=Tom |last3=Conen |first3=Franz |last4=Dobbie |first4=Karen E. |last5=Massheder |first5=Jonathan |last6=Rey |first6=Ana |journal=European Journal of Soil Science |volume=69 |issue=1 |title=Exchange of greenhouse gases between soil and atmosphere: interactions of soil physical factors and biological processes |url=https://www.researchgate.net/publication/322575479 |date=January 2018 |pages=10–20 |doi=10.1111/ejss.12539 |access-date=17 November 2025 }}</ref> [[Soil texture]] and [[soil structure|structure]] strongly affect soil porosity and gas diffusion. It is the total pore space ([[porosity]]) of soil, not the pore size, and the degree of pore interconnection (or conversely pore sealing), together with water content, air [[turbulence]] and temperature, that determine the rate of diffusion of gases into and out of soil.{{sfn|Russell|1957|pp=35–36}}<ref name="Smith2003"/> [[Ped#Platy|Platy]] soil structure and soil compaction (low porosity) impede gas flow, and a deficiency of oxygen may encourage [[anaerobic bacteria]] to reduce (strip oxygen) from [[nitrate]] NO<sub>3</sub> to the gases N<sub>2</sub>, N<sub>2</sub>O, and NO, which are then lost to the atmosphere, thereby depleting the soil of nitrogen, a detrimental process called [[denitrification]].<ref>{{cite journal |last1=Ruser |first1=Reiner |last2=Flessa |first2=Heiner |last3=Russow |first3=Rolf |last4=Schmidt |first4=G. |last5=Buegger |first5=Franz |last6=Munch |first6=J.C. |journal=[[Soil Biology and Biochemistry]] |volume=38 |issue=2 |title=Emission of N<sub>2</sub>O, N<sub>2</sub> and CO<sub>2</sub> from soil fertilized with nitrate: effect of compaction, soil moisture and rewetting |url=https://downloads.regulations.gov/APHIS-2011-0023-0105/attachment_4.pdf |date=February 2006 |pages=263–74 |doi=10.1016/j.soilbio.2005.05.005 |access-date=17 November 2025 }}</ref> Aerated soil is also a net sink of [[methane]] (CH<sub>4</sub>)<ref>{{cite journal |last1=Hartmann |first1=Adrian A. |last2=Buchmann |first2=Nina |last3=Niklaus |first3=Pascal A. |journal=[[Plant and Soil]] |volume=342 |issue=1–2 |title=A study of soil methane sink regulation in two grasslands exposed to drought and N fertilization |date=21 December 2010 |pages=265–75 |doi=10.1007/s11104-010-0690-x |bibcode=2011PlSoi.342..265H |hdl=20.500.11850/34759 |s2cid=25691034 |url=https://fr.1lib.sk/book/39985431/0410d9 |access-date=17 November 2025 }}</ref> but a net producer of [[methane]] (a strong heat-trapping [[greenhouse gas]]) when soils are depleted of oxygen and subject to elevated temperatures.<ref>{{cite journal |last1=Moore |first1=Tim R. |last2=Dalva |first2=Moshe |journal=Journal of Soil Science |volume=44 |issue=4 |title=The influence of temperature and water table position on carbon dioxide and methane emissions from laboratory columns of peatland soils |url=https://www.researchgate.net/publication/229878721 |date=December 1993 |pages=651–64 |doi=10.1111/j.1365-2389.1993.tb02330.x |bibcode=1993EuJSS..44..651M |access-date=17 November 2025 }}</ref>

Soil atmosphere is also the seat of emissions of [[Volatile (astrogeology)|volatiles]] other than carbon and nitrogen oxides from various soil organisms, e.g. roots,<ref>{{cite journal |last1=Hiltpold |first1=Ivan |last2=Toepfer |first2=Stefan |last3=Kuhlmann |first3=Ulrich |last4=Turlings |first4=Ted C.J. |journal=Chemoecology |volume=20 |issue=2 |title=How maize root volatiles affect the efficacy of entomopathogenic nematodes in controlling the western corn rootworm? |url=https://www.researchgate.net/publication/215470509 |date=22 December 2009 |pages=155–62 |doi=10.1007/s00049-009-0034-6 |bibcode=2010Chmec..20..155H |s2cid=30214059 |access-date=17 November 2025 }}</ref> bacteria,<ref>{{cite journal |last1=Ryu |first1=Choong-Min |last2=Farag |first2=Mohamed A. |last3=Hu |first3=Chia-Hui |last4=Reddy |first4=Munagala S. |last5= Wei |first5= Han-Xun |last6= Paré |first6=Paul W. |last7= Kloepper |first7= Joseph W. |journal=[[Proceedings of the National Academy of Sciences of the United States of America]] |volume=100 |issue=8 |title=Bacterial volatiles promote growth in ''Arabidopsis'' |date=8 April 2003 |pages=4927–32 |doi=10.1073/pnas.0730845100 |pmid=12684534 |pmc=153657 |bibcode=2003PNAS..100.4927R |url=https://www.academia.edu/70002424 |access-date=17 November 2025 }}</ref> fungi,<ref>{{cite journal |last1=Hung |first1=Richard |last2=Lee |first2=Samantha |last3=Bennett |first3=Joan W. |journal=[[Applied Microbiology and Biotechnology]] |volume=99 |issue=8 |title=Fungal volatile organic compounds and their role in ecosystems |url=https://www.researchgate.net/publication/273638498 |date=14 March 2015 |pages=3395–405 |doi=10.1007/s00253-015-6494-4 |pmid=25773975 |s2cid=14509047 |access-date=17 November 2025 }}</ref> animals.<ref>{{cite journal |last1=Purrington |first1=Foster Forbes |last2=Kendall |first2=Paricia A. |last3=Bater |first3=John E. |last4=Stinner |first4=Benjamin R. |journal=Great Lakes Entomologist |volume=24 |issue=2 |title=Alarm pheromone in a gregarious poduromorph collembolan (Collembola: Hypogastruridae) |year=1991 |pages=75–8 |doi=10.22543/0090-0222.1732 |doi-access=free }}</ref> These volatiles are used as chemical cues, making soil atmosphere the seat of interaction networks<ref>{{cite journal |last1=Badri |first1=Dayakar V. |last2=Weir |first2=Tiffany L. |last3=Van der Lelie |first3=Daniel |last4=Vivanco |first4=Jorge M |journal=[[Current Opinion in Biotechnology]] |volume=20 |issue=6 |title=Rhizosphere chemical dialogues: plant–microbe interactions |url=https://www.bicga.org.uk/docs/Rhizosphere_chemical_dialogues_plant.pdf |doi=10.1016/j.copbio.2009.09.014 |pmid=19875278 |date=December 2009 |pages=642–50 |access-date=17 November 2025 |archive-date=21 September 2022 |archive-url=https://web.archive.org/web/20220921224421/http://www.bicga.org.uk/docs/Rhizosphere_chemical_dialogues_plant.pdf |url-status=live }}</ref><ref>{{cite journal |last1=Salmon |first1=Sandrine |last2=Ponge |first2=Jean-François |journal=[[Soil Biology and Biochemistry]] |volume=33 |issue=14 |title=Earthworm excreta attract soil springtails: laboratory experiments on Heteromurus nitidus (Collembola: Entomobryidae) |url=https://www.academia.edu/20508985 |doi=10.1016/S0038-0717(01)00129-8 |date=November 2001 |pages=1959–69 |bibcode=2001SBiBi..33.1959S |s2cid=26647480 |access-date=17 November 2025 }}</ref> playing a decisive role in the stability, dynamics and evolution of soil ecosystems.<ref>{{cite journal |last1=Lambers |first1=Hans |last2=Mougel |first2=Christophe |last3=Jaillard |first3=Benoît |last4=Hinsinger |first4=Philipe |journal=[[Plant and Soil]] |volume=321 |issue=1–2 |title=Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective |url=https://www.academia.edu/25517742 |doi=10.1007/s11104-009-0042-x |date=20 June 2009 |pages=83–115 |bibcode=2009PlSoi.321...83L |s2cid=6840457 |access-date=17 November 2025 }}</ref> [[Biogenic substance|Biogenic]] soil [[volatile organic compound]]s are exchanged with the aboveground atmosphere, in which they are just 1–2 orders of magnitude lower than those from aboveground vegetation.<ref>{{cite journal |last1=Peñuelas |first1=Josep |last2=Asensio |first2=Dolores |last3=Tholl |first3=Dorothea |last4=Wenke |first4=Katrin |last5=Rosenkranz |first5=Maaria |last6=Piechulla |first6=Birgit |last7=Schnitzler |first7=Jörg-Petter |journal=[[Plant, Cell and Environment]] |volume=37 |issue=8 |title=Biogenic volatile emissions from the soil |date=August 2014 |pages=1866–91 |doi=10.1111/pce.12340 |pmid=24689847 |doi-access=free |bibcode=2014PCEnv..37.1866P }}</ref>

Humans can get some idea of the soil atmosphere through the well-known 'after-the-rain' scent, when infiltering rainwater flushes out the whole soil atmosphere after a drought period, or when soil is excavated,<ref>{{cite journal |last1=Buzuleciu |first1=Samuel A. |last2=Crane |first2=Derek P. |last3=Parker |first3=Scott L. |journal=[[Herpetological Conservation and Biology]] |volume=11 |issue=3 |title=Scent of disinterred soil as an olfactory cue used by raccoons to locate nests of diamond-backed terrapins (''Malaclemys terrapin'') |url=https://www.herpconbio.org/Volume_11/Issue_3/Buzuleciu_etal_2016.pdf |date=16 December 2016 |pages=539–51 |access-date=17 November 2025 }}</ref> a bulk property attributed in a [[reductionist]] manner to particular [[biochemical]] compounds such as [[petrichor]] or [[geosmin]].

== Solid phase (soil matrix) ==
{{main|Soil matrix}}
Soil particles can be classified by their chemical composition ([[mineralogy]]) as well as their size. The [[Particle-size distribution|particle size distribution]] of a soil, its [[soil texture|texture]], determines many of the properties of that soil, in particular [[hydraulic conductivity]] and [[water potential]],<ref>{{cite journal |last1=Saxton |first1=Keith E. |last2=Rawls |first2=Walter J. |journal=[[Soil Science Society of America Journal]] |volume=70 |issue=5 |title=Soil water characteristic estimates by texture and organic matter for hydrologic solutions |url=https://www.atmos.illinois.edu/~sshu3/model/saxton2006.pdf |archive-url=https://web.archive.org/web/20180902183902/https://pdfs.semanticscholar.org/5e63/c886c4f68af5e5c242c006d2d882f0a65bfe.pdf |url-status=live |archive-date=2 September 2018 |date=September 2006 |pages=1569–78 |doi=10.2136/sssaj2005.0117 |access-date=17 November 2025 |bibcode=2006SSASJ..70.1569S |s2cid=16826314 }}</ref> but the [[mineralogy]] of those particles can strongly modify those properties. The mineralogy of the finest soil particles, [[Clay mineral|clay]], is especially important.<ref>{{cite journal |last=Grim |first=Ralph E. |journal=[[Science (journal)|Science]] |volume=135 |issue=3507 |title=Clay mineralogy |url=https://fr.1lib.sk/book/54826330/0c2dba |date=16 March 1962 |pages=890–8 |doi=10.1126/science.135.3507.890 |access-date=17 November 2025 }}</ref>

== Soil biodiversity ==
{{main|Soil biology}}
Large numbers of [[Microorganism|microbes]], [[animal]]s, [[plant]]s and [[Fungus|fungi]] are living in soil.<ref>{{cite book |last1=Dessaux |first1=Yves |last2=Chapelle |first2=Émilie |last3=Faure |first3=Denis |date=20 September 2010 |chapter=Quorum sensing and quorum quenching in soil ecosystems |title=Biocommunication in soil microorganisms |edition=1st |editor-last=Witzany |editor-first=Günther |publisher=[[Springer Nature]] |location=Berlin, Germany |pages=339–67 |isbn=978-3-642-14512-4 |chapter-url=https://www.researchgate.net/publication/225865218 |doi=10.1007/978-3-642-14512-4_13 |access-date=18 November 2025 }}</ref> However, [[biodiversity]] in soil is much harder to study as most of this life is invisible, hence estimates about soil biodiversity have been unsatisfactory. A recent study suggested that soil is likely home to 59 ± 15% of the species on Earth. [[Enchytraeidae]] (potworms) have the greatest percentage of their species living in soil (98.6%), followed by fungi (90%), plants (85.5%), and termites ([[Termite|Isoptera]]) (84.2%). Many other groups of animals have substantial fractions of species living in soil, e.g. about 30% of [[insect]]s, and close to 50% of [[arachnid]]s.<ref>{{cite journal |last1=Anthony |first1=Mark A. |last2=Bender |first2=S. Franz |last3=Van der Heijden |first3=Marcel G. A. |date=15 August 2023 |title=Enumerating soil biodiversity |journal=[[Proceedings of the National Academy of Sciences of the United States of America]] |language=en |volume=120 |issue=33 |article-number=e2304663120 |doi=10.1073/pnas.2304663120 |pmid=37549278 |pmc=10437432 |bibcode=2023PNAS..12004663A |issn=0027-8424 |doi-access=free }}</ref> While most [[vertebrate]]s live above ground (ignoring aquatic species), many species are [[fossorial]], that is, they live in soil (e.g. [[Mole (animal)|mole]]s, [[pocket gopher]]s, [[vole]]s, [[Scolecophidia|blind snakes]]), an adaptation to subterranean life thought to be inherited from past global [[Ecological crisis|ecological crise]]s.<ref>{{cite journal |last1=Marchetti |first1=Lorenzo |last2=MacDougall |first2=Mark J. |last3=Buchwitz |first3=Michael |last4=Canoville |first4=Aurore |last5=Herde |first5=Max |last6=Kammerer |first6=Christian F. |last7=Fröbisch |first7=Jörg |journal=[[Earth-Science Reviews]] |volume=250 |article-number=104702 |title=Origin and early evolution of vertebrate burrowing behaviour |date=March 2024 |doi=10.1016/j.earscirev.2024.104702 |url=https://archive.org/details/marchetti-et-al.-2024 |access-date=18 November 2025 }}</ref>

== Chemistry ==
{{for|the academic discipline|Soil chemistry}}
The chemistry of a soil determines its ability to supply available [[Plant nutrition|plant nutrients]] and affects its physical properties and the health of its living population. In addition, a soil's chemistry also determines its [[corrosivity]], stability, and ability to [[Sorption|absorb]] [[pollutants]] and to filter water. It is the [[surface chemistry]] of mineral and organic [[colloids]] that determines soil's chemical properties.<ref>{{cite book |last=Sposito |first=Garrison |date=1984 |title=The surface chemistry of soils |publisher=[[Oxford University Press]] |location=New York, New York |url=https://fr.1lib.sk/book/868167/dcb874 |access-date=18 November 2025 }}</ref> A colloid is a small, insoluble particle ranging in size from 1 [[nanometer]] to 1 [[micrometre|micrometer]], thus small enough to remain suspended by [[Brownian motion]] in a fluid medium without settling.<ref>{{cite web |last=Wynot |first=Christopher |title=Theory of diffusion in colloidal suspensions |url=https://www.owlnet.rice.edu/~ceng402/proj02/cwynot/402project.htm |access-date=18 November 2025 }}</ref> Most soils contain organic colloidal particles called [[humus]] as well as the inorganic colloidal particles of [[Clay mineral|clay]]s. The very high [[specific surface area]] of colloids and their net [[electrical charge]]s give soil its ability to hold and release [[ions]]. Negatively charged sites on colloids attract and release [[cations]] in what is referred to as [[cation exchange]]. [[Cation-exchange capacity]] is the amount of exchangeable [[cations]] per unit weight of dry soil and is expressed in terms of [[milliequivalents]] of [[positively charged]] ions per 100&nbsp;grams of soil (or centimoles of positive charge per kilogram of soil; [[Cation-exchange capacity|cmol<sub>c</sub>/kg]]). Similarly, positively charged sites on colloids can attract and release [[anions]] in the soil, giving the soil [[anion-exchange capacity]].

=== Cation and anion exchange ===
{{Further|Cation-exchange capacity}}
The [[cation exchange]], that takes place between colloids and soil water, [[Buffer solution|buffers]] (moderates) [[soil pH]],<ref>{{cite journal |last1=Nelson |first1=Paul N. |last2=Su |first2=Ninghu |journal=[[Australian Journal of Soil Research]] |volume=48 |issue=3 |pages=201–7 |title=Soil pH buffering capacity: a descriptive function and its application to some acidic tropical soils |date=6 May 2010 |doi=10.1071/SR09150 |url=https://www.researchgate.net/publication/236878026 |access-date=18 November 2025 }}</ref> alters [[soil structure]],<ref>{{cite journal |last1=Dimoyiannis |first1=D. G. |last2=Tsadilas |first2=Christos D. |last3=Valmis |first3=S. |journal=Communications in Soil Science and Plant Analysis |volume=29 |issue=9–10 |title=Factors affecting aggregate instability of Greek agricultural soils |url=https://www.researchgate.net/publication/233123204 |doi=10.1080/00103629809370023 |year=1998 |pages=1239–51 |access-date=18 November 2025 }}</ref> and purifies [[Percolation|percolating]] water by [[Adsorption|adsorbing]] cations of all types, both useful and harmful.<ref>{{cite journal |last1=Meetei |first1=Thounaojam Thomas |last2=Devi |first2= Yumnam Bijilaxmi |last3=Chanu |first3=Thounaojam Thorny |journal=International Research Journal of Pure and Applied Chemistry |volume=21 |issue=6 |title=Ion exchange: the most important chemical reaction on Earth after photosynthesis |url=https://www.researchgate.net/publication/341122984 |doi=10.9734/IRJPAC/2020/v21i630174 |date=4 May 2020 |pages=31–42 |access-date=18 November 2025 }}</ref>

The negative or positive charges on colloid particles make them able to hold cations or anions, respectively, to their surfaces. The charges result from four sources.{{sfn|Donahue|Miller|Shickluna|1977|p=103–106}}

# [[Isomorphous replacement|Isomorphous]] substitution occurs in clay during its formation, when lower-[[Valence (chemistry)|valence]] cations substitute for higher-valence cations in the [[crystal structure]].<ref>{{cite journal |last1=Sposito |first1= Garrison |last2=Skipper |first2=Neal T. |last3=Sutton |first3=Rebecca |last4=Park |first4=Sung-Ho |last5=Soper |first5=Alan K. |last6=Greathouse |first6=Jeffery A. |journal=[[Proceedings of the National Academy of Sciences of the United States of America]] |volume=96 |issue=7 |title=Surface geochemistry of the clay minerals |date=30 March 1999 |pages=3358–64 |doi=10.1073/pnas.96.7.3358 |pmid=10097044 |bibcode=1999PNAS...96.3358S |pmc=34275 |doi-access=free }}</ref> Substitutions in the outermost layers are more effective than for the innermost layers, as the [[electric charge]] strength drops off as the square of the distance. The net result is oxygen atoms with net negative charge and the ability to attract cations.<ref>{{cite journal |last1=Wang |first1=Qian |last2=Zhu |first2=Chang |last3=Yun |first3=Jiena |last4=Yang |first4=Gang |date=14 November 2017 |title=Isomorphic substitutions in clay materials and adsorption of metal ions onto external surfaces: a DFT investigation |journal=[[The Journal of Physical Chemistry C]] |volume=121 |issue=48 |pages=26722–32 |url=https://fr.1lib.sk/book/99017309/4372bc |doi=10.1021/acs.jpcc.7b03488 |access-date=18 November 2025 }}</ref>
# Edge-of-clay oxygen atoms are not in balance ionically as the [[Tetrahedral molecular geometry|tetrahedral]] and [[Octahedral molecular geometry|octahedral]] structures are incomplete.<ref>{{cite journal |last1=Bickmore |first1=Barry R. |last2=Rosso |first2=Kevin M. |last3=Nagy |first3=Kathryn L. |last4=Cygan |first4=Randall T. |last5=Tadanier |first5=Christopher J. |year=2003 |title=Ab initio determination of edge surface structures for dioctahedral 2:1 phyllosilicates: implications for acid-base reactivity |journal=[[Clays and Clay Minerals]] |volume=51 |issue=4 |pages=359–71 |url=https://randallcygan.com/wp-content/uploads/2017/06/Bickmore2003CCM.pdf |doi=10.1346/CCMN.2003.0510401 |access-date=18 November 2025 |bibcode=2003CCM....51..359B |s2cid=97428106 }}</ref>
# [[Hydroxyl]]s may substitute for oxygens of the silica layers, a process called [[hydroxylation]]. When the hydrogens of the clay hydroxyls are ionised into solution, they leave the oxygen with a negative charge (anionic clays).<ref>{{cite journal |last1=Rajamathi |first1=Michael |last2=Thomas |first2=Grace S. |last3=Kamath |first3=P. Vishnu |date=October 2001 |title=The many ways of making anionic clays |journal=[[Journal of Chemical Sciences]] |volume=113 |issue=5–6 |pages=671–80 |doi=10.1007/BF02708799 |s2cid=97507578 |url=https://www.academia.edu/56207482 |access-date=18 November 2025 }}</ref>
# Hydrogens of humus hydroxyl groups may also be ionised into solution, leaving, similarly to clay, an oxygen with a negative charge.<ref>{{cite journal |last1=Moayedi |first1=Hossein |last2=Kazemian |first2=Sina |date=30 January 2013 |title=Zeta potentials of suspended humus in multivalent cationic saline solution and its effect on electro-osomosis behavior |journal=Journal of Dispersion Science and Technology |volume=34 |issue=2 |pages=283–94 |url=https://www.academia.edu/10587240 |doi=10.1080/01932691.2011.646601 |s2cid= 94333872 |access-date=18 November 2025 }}</ref>

Cations held to the negatively charged colloids resist being washed downward by water and are at first out of reach of plant roots, thereby preserving the [[soil fertility]] in areas of moderate rainfall and low temperatures.<ref>{{cite web |last=Pettit |first=Robert E. |title=Organic matter, humus, humate, humic acid, fulvic acid and humin: their importance in soil fertility and plant health |url=https://humates.com/wp-content/uploads/2020/04/ORGANICMATTERPettit.pdf |access-date=18 November 2025 }}</ref><ref>{{cite journal |last1=Diamond |first1=Sidney |last2=Kinter |first2=Earl B. |year=1965 |title=Mechanisms of soil-lime stabilization: an interpretive review |journal=Highway Research Record |volume=92 |pages=83–102 |url=https://onlinepubs.trb.org/onlinepubs/hrr/1965/92/92-006.pdf |access-date=18 November 2025 }}</ref>

There is a hierarchy in the process of cation exchange on colloids, as cations differ in the strength of adsorption by the colloid and hence their ability to replace one another ([[ion exchange]]). If present in equal amounts in the soil water solution:

Al<sup>3+</sup> replaces H<sup>+</sup> replaces Ca<sup>2+</sup> replaces Mg<sup>2+</sup> replaces K<sup>+</sup> same as {{chem|NH|4|+}} replaces Na<sup>+</sup><ref>{{cite journal |last=Woodruff |first=Clarence M. |date=April 1955 |title=The energies of replacement of calcium by potassium in soils |journal=[[Soil Science Society of America Journal]] |volume=19 |issue=2 |pages=167–71 |doi=10.2136/sssaj1955.03615995001900020014x |url=https://fr.1lib.sk/book/110840298/b4d8cf |bibcode=1955SSASJ..19..167W |access-date=18 November 2025 }}</ref>

If one cation is added in large amounts, it may replace the others by the [[Shear force|sheer force]] of its numbers. This is called [[law of mass action]]. This is largely what occurs with the addition of cationic [[Fertilizer|fertilisers]] ([[potash]], [[Lime (material)|lime]]).<ref>{{cite book |last1=Hendershot |first1=William H. |last2=Lalande |first2=Hélène |last3=Duquette |first3=Martin |title=Soil sampling and methods of analysis |year=2007 |publisher=[[CRC Press]] |isbn=9781420005271 |editor-last1=Carter |editor-first1=Martin R. |editor-last2=Gregorich |editor-first2=Edward G. |edition=2nd |location=Boca raton, Florida |pages=197–206 |chapter=Ion exchange and exchangeable cations |chapter-url=https://books.google.fr/books/content?id=ZTJsbXsikagC&hl=fr&pg=PA197&img=1&zoom=3&ots=VhFyyS_YR2&sig=ACfU3U0Oq3owsrnuZ2lynufUBZblcogVJw&w=1280 |access-date=19 November 2025 }}</ref>

As the soil solution becomes more acidic (low [[pH]], meaning an abundance of H<sup>+</sup>), the other cations more weakly bound to colloids are pushed into solution as hydrogen ions occupy exchange sites ([[protonation]]). A low pH may cause the hydrogen of hydroxyl groups to be pulled into solution, leaving charged sites on the colloid available to be occupied by other cations. This [[Ionization|ionisation]] of [[hydroxy group]]s on the surface of soil colloids creates what is described as pH-dependent [[surface charge]]s.<ref>{{cite journal |last1=Bolland |first1=Mike D. A. |last2=Posner |first2=Alan M. |last3=Quirk |first3=James P. |year=1980 |title=pH-independent and pH-dependent surface charges on kaolinite |journal=[[Clays and Clay Minerals]] |volume=28 |issue=6 |pages=412–8 |doi=10.1346/CCMN.1980.0280602 |bibcode=1980CCM....28..412B |s2cid=12462516 |url=https://www.researchgate.net/publication/237294635 |access-date=19 November 2025 }}</ref> Unlike permanent charges developed by [[Isomorphous replacement|isomorphous substitution]], pH-dependent charges are variable and increase with increasing pH.<ref>{{cite web |last=Chakraborty |first=Somsubhra |url=http://elearn.psgcas.ac.in/nptel/courses/video/126105016/lec24.pdf |date=2 February 2019 |title=Cation exchange capacity (CEC) |access-date=19 November 2025 }}</ref> Freed cations can be made available to plants but are also prone to be leached from the soil, possibly making the soil less fertile.<ref>{{cite journal |last1=Silber |first1=Avner |last2=Levkovitch |first2=Irit |last3= Graber |first3=Ellen R. |year=2010 |title=pH-dependent mineral release and surface properties of cornstraw biochar: agronomic implications |journal=[[Environmental Science and Technology]] |volume=44 |issue=24 |pages=9318–23 |url=https://www.academia.edu/24532141 |doi=10.1021/es101283d |pmid=21090742 |access-date=19 November 2025 |bibcode=2010EnST...44.9318S }}</ref> Plants are able to excrete H<sup>+</sup> into the soil through the synthesis of [[organic acid]]s and by that means, change the pH of the soil near the root and push cations off the colloids, thus making those available to the plant.<ref>{{cite journal |last1=Dakora |first1=Felix D. |last2=Phillips |first2=Donald D. |date=August 2002 |title=Root exudates as mediators of mineral acquisition in low-nutrient environments |journal=[[Plant and Soil]] |volume=245 |issue=1 |pages=35–47 |url=https://www.researchgate.net/publication/225265745 |doi=10.1023/A:1020809400075 |bibcode=2002PlSoi.245...35D |s2cid=3330737 |access-date=19 November 2025 |archive-url=https://web.archive.org/web/20190819123707/http://www.plantstress.com/articles/min_deficiency_i/root_exudates.pdf |archive-date=19 August 2019 |url-status=live }}</ref>

==== Cation exchange capacity (CEC) ====

[[Cation exchange capacity]] is the soil's ability to remove cations from the soil water solution and sequester those to be exchanged later as the plant roots release hydrogen ions to the solution.<ref>{{cite journal |last=Brown |first=John C. |date=December 1978 |title=Mechanism of iron uptake by plants |journal=[[Plant, Cell & Environment|Plant, Cell and Environment]] |volume=1 |issue=4 |pages=249–57 |doi=10.1111/j.1365-3040.1978.tb02037.x |bibcode=1978PCEnv...1..249B |url=https://fr.1lib.sk/book/41304841/1381d1 |access-date=19 November 2025 }}</ref> CEC is the amount of exchangeable hydrogen cations (H<sup>+</sup>) that will combine with 100&nbsp;grams dry weight of soil and whose measure is one [[milliequivalent]] per 100&nbsp;grams of soil (1&nbsp;meq/100&nbsp;g). Hydrogen ions have a single charge and one-thousandth  of a gram (1 mg) of hydrogen ions per 100&nbsp;grams dry soil gives a measure of one milliequivalent of hydrogen ion. Calcium, with an atomic weight 40 times that of hydrogen and with a [[Valence (chemistry)|valence]] of two, converts to {{nowrap|(40 ÷ 2) × 1 milliequivalent}} = 20 milliequivalents of hydrogen ion per 100&nbsp;grams of dry soil or 20&nbsp;meq/100&nbsp;g.{{sfn|Donahue|Miller|Shickluna|1977|p=114}} The modern measure of CEC is expressed as centimoles of positive charge per kilogram (cmol/kg) of oven-dry soil.

Most of the soil's CEC occurs on clay and humus colloids, and the lack of those in hot, humid, wet climates (such as [[tropical rainforest]]s), due to fast leaching and decomposition, respectively, explains the apparent lack of [[soil fertility|fertility]] of tropical soils.<ref>{{cite journal |last1=Singh |first1=Jamuna Sharan |last2=Raghubanshi |first2=Akhilesh Singh |last3=Singh |first3=Raj S. |last4=Srivastava |first4=Sanjai C. |date=6 April 1989 |title=Microbial biomass acts as a source of plant nutrient in dry tropical forest and savanna |journal=[[Nature (journal)|Nature]] |volume=338 |issue=6215 |pages=499–500 |url=https://www.researchgate.net/publication/236941524 |doi=10.1038/338499a0 |access-date=19 November 2025 |bibcode=1989Natur.338..499S |s2cid=4301023 }}</ref> Live plant roots also have some CEC, linked to their [[specific surface area]].<ref>{{cite journal |last1=Szatanik-Kloc |first1=Alicja |last2=Szerement |first2=Justyna |last3=Józefaciuk |first3=Grzegorz |date=August 2017 |title=The role of cell walls and pectins in cation exchange and surface area of plant roots |journal=[[Journal of Plant Physiology]] |volume=215 |pages=85–90 |url=https://daneshyari.com/article/preview/5517999.pdf |doi=10.1016/j.jplph.2017.05.017 |pmid=28600926 |bibcode=2017JPPhy.215...85S |access-date=19 November 2025 }}</ref>

{| class="wikitable" style="border-spacing: 5px; margin:auto;"
|+ Cation exchange capacity for soils; soil textures; soil colloids{{sfn|Donahue|Miller|Shickluna|1977|pp=115–116}}
|-
! scope="col" style="width:200px;"| Soil
! scope="col" style="width:100px;"| State
! scope="col" style="width:100px;"| CEC meq/100&nbsp;g
|-
| Charlotte fine sand ||Florida|| 1.0
|-
| Ruston fine sandy loam ||Texas|| 1.9
|-
| Glouchester loam ||New Jersey || 11.9
|-
| Grundy silt loam || Illinois || 26.3
|-
| Gleason clay loam || California || 31.6
|-
| Susquehanna clay loam || Alabama || 34.3
|-
| Davie mucky fine sand || Florida || 100.8
|-
| Sands || {{n/a}} || 1–5
|-
| Fine sandy loams || {{n/a}} || 5–10
|-
| Loams and silt loams || {{n/a}} || 5–15
|-
| Clay loams || {{n/a}} || 15–30
|-
| Clays || {{n/a}} || over 30
|-
| Sesquioxides || {{n/a}} || 0–3
|-
| Kaolinite || {{n/a}} || 3–15
|-
| Illite || {{n/a}} || 25–40
|-
| Montmorillonite || {{n/a}} || 60–100
|-
| Vermiculite (similar to illite) || {{n/a}} || 80–150
|-
| Humus || {{n/a}} || 100–300
|}

==== Anion exchange capacity (AEC) ====

Anion exchange capacity is the soil's ability to remove anions (such as [[nitrate]], [[phosphate]]) from the soil water solution and sequester those for later exchange as the plant roots release carbonate anions to the soil water solution.<ref name="Hinsinger2001">{{cite journal |last=Hinsinger |first=Philippe |date=December 2001 |title=Bioavailability of soil inorganic P in the rhizosphere as affected by root-induced chemical changes: a review |journal=[[Plant and Soil]] |volume=237 |issue=2 |pages=173–95 |doi=10.1023/A:1013351617532 |bibcode=2001PlSoi.237..173H |s2cid=8562338 |url=https://www.researchgate.net/publication/225852665 |access-date=19 November 2025 }}</ref> Those colloids which have low [[Cation-exchange capacity|CEC]] tend to have some AEC. [[Amorphous solid|Amorphous]] and [[sesquioxide]] clays have the highest AEC,<ref>{{cite report |last1=Gu |first1=Baohua |last2=Schulz |first2=Robert K. |title=Anion retention in soil: possible application to reduce migration of buried technetium and iodine, a review |date=October 1991 |doi=10.2172/5980032 |s2cid=91359494 |url=https://www.osti.gov/servlets/purl/5980032 |access-date=19 November 2025 }}</ref> followed by the iron oxides.<ref>{{cite journal |last1=Lawrinenko |first1=Michael |last2=Jing |first2=Dapeng |last3=Banik |first3=Chumki |last4=Laird |first4=David A. |date=July 2017 |title=Aluminum and iron biomass pretreatment impacts on biochar anion exchange capacity |journal=[[Carbon (journal)|Carbon]] |volume=118 |pages=422–30 |doi=10.1016/j.carbon.2017.03.056 |bibcode=2017Carbo.118..422L |url=https://www.academia.edu/90757446 |access-date=19 November 2025 }}</ref> Levels of AEC are much lower than for CEC, because of the generally higher rate of positively (versus negatively) charged surfaces on soil colloids, to the exception of variable-charge soils.<ref>{{cite journal |last1=Sollins |first1=Phillip |last2=Robertson |first2=G. Philip |last3=Uehara |first3=Goro |date=October 1988 |title=Nutrient mobility in variable- and permanent-charge soils |journal=Biogeochemistry |volume=6 |issue=3 |pages=181–99 |url=https://lter.kbs.msu.edu/docs/robertson/Sollins_et_al._1988_Biogeochemistry.pdf |doi=10.1007/BF02182995 |bibcode=1988Biogc...6..181S |s2cid=4505438 |access-date=19 November 2025 }}</ref> Phosphates tend to be held at anion exchange sites.<ref>{{cite journal |last=Sanders |first=W. M. H. |year=1964 |title=Extraction of soil phosphate by anion-exchange membrane |journal=New Zealand Journal of Agricultural Research |volume=7 |issue=3 |pages=427–31 |doi=10.1080/00288233.1964.10416423 |bibcode=1964NZJAR...7..427S |url=https://fr.1lib.sk/book/62224844/3b60b6 |access-date=19 November 2025 }}</ref>

Iron and aluminum [[hydroxide]] clays are able to exchange their hydroxide anions (OH<sup>−</sup>) for other anions.<ref name="Hinsinger2001"/> The order reflecting the strength of anion adhesion is as follows:

:{{chem|H|2|PO|4|−}} replaces {{chem|SO|4|2−}} replaces {{chem|NO|3|−}} replaces Cl<sup>−</sup>

The amount of exchangeable anions is of a magnitude of tenths to a few milliequivalents per 100&nbsp;g dry soil.{{sfn|Donahue|Miller|Shickluna|1977|pp=115–116}} As pH rises, there are relatively more hydroxyls, which will displace anions from the colloids and force them into solution and out of storage; hence AEC decreases with increasing pH (alkalinity).<ref>{{cite journal |last1=Lawrinenko |first1=Mike |last2=Laird |first2=David A. |year=2015 |title=Anion exchange capacity of biochar |journal=[[Green Chemistry (journal)|Green Chemistry]] |volume=17 |issue=9 |pages=4628–36 |doi=10.1039/C5GC00828J |s2cid=52972476 |url=https://fr.1lib.sk/book/77675834/d2350d |access-date=19 November 2025 }}</ref>

=== Reactivity (pH) ===
{{Main|Soil pH|Soil pH#Effect of soil pH on plant growth}}
Soil reactivity is expressed in terms of pH and is a measure of the [[Acidity or alkalinity|acidity]] or [[alkalinity]] of the soil. More precisely, it is a measure of [[hydronium]] concentration in an aqueous solution and ranges in values from 0 to 14 (acidic to basic) but practically speaking for soils, pH ranges from 3.5 to 9.5, as pH values beyond those extremes are toxic to life forms.<ref>{{cite web |last=Robertson |first=Bryan |title=pH requirements of freshwater aquatic life |url=https://www.waterboards.ca.gov/waterrights/water_issues/programs/bay_delta/deltaflow/docs/exhibits/bigbreak/dscbb_exh5.pdf |access-date=19 November 2025 |archive-date=8 May 2021 |archive-url=https://web.archive.org/web/20210508070517/https://www.waterboards.ca.gov/centralvalley/water_issues/basin_plans/ph_turbidity/ph_turbidity_04phreq.pdf |url-status=live }}</ref>

At 25&nbsp;°C an aqueous solution that has a pH of 3.5 has 10<sup>−3.5</sup> [[mole (unit)|moles]] H<sub>3</sub>O<sup>+</sup> (hydronium ions) per litre of solution (and also 10<sup>−10.5</sup> moles per litre OH<sup>−</sup>). A pH of 7, defined as neutral, has 10<sup>−7</sup> moles of hydronium ions per litre of solution and also 10<sup>−7</sup> moles of OH<sup>−</sup> per litre; since the two concentrations are equal, they are said to neutralise each other. A pH of 9.5 has 10<sup>−9.5</sup> moles hydronium ions per litre of solution (and also 10<sup>−2.5</sup> moles per litre OH<sup>−</sup>). A pH of 3.5 has one million times more hydronium ions per litre than a solution with pH of 9.5 ({{nowrap|9.5 − 3.5 {{=}} 6}} or 10<sup>6</sup>) and is thus more acidic.<ref>{{cite book |editor-last=Chang |editor-first=Raymond |title=Chemistry |date=2010 |edition=12th |url=https://www.academia.edu/44394574 |publisher=[[McGraw-Hill]] |location=New York, New York |isbn=978-0-07-802151-0 |page=666 |access-date=19 November 2025 }}</ref>

The effect of pH on a soil is to remove from the soil or to make available certain ions. Soils with high acidity tend to have toxic amounts of [[aluminium]] and [[manganese]].<ref>{{cite journal |last1=Rajamathi |first1=Michael |last2=Thomas |first2=Grace S. |last3=Kamath |first3=P. Vishnu |date=October 2001 |title=The many ways of making anionic clays |journal=[[Journal of Chemical Sciences]] |volume=113 |issue=5–6 |pages=671–80 |doi=10.1007/BF02708799 |s2cid=97507578 |url=https://www.researchgate.net/publication/226095576 |access-date=19 November 2025 }}</ref> As a result of a trade-off between [[toxicity]] and requirement most nutrients are better available to plants at moderate pH,<ref>{{cite book |last1=Läuchli |first1=André |last2=Grattan |first2=Steve R. |year=2012 |chapter=Soil pH extremes |title=Plant stress physiology |edition=1st |editor-first=Sergey |editor-last=Shabala |publisher=[[CAB International]] |location=Wallingford, United Kingdom |pages=194–209 |isbn=978-1-84593-995-3 |chapter-url=https://www.researchgate.net/publication/269112359 |doi=10.1079/9781845939953.0194 |access-date=19 November 2025 }}</ref> although most minerals are more soluble ([[Weathering|weatherable]]) in acid soils.<ref>{{cite journal |last1=Drever |first1=James I. |last2=Stillings |first2=Lisa L. |date=21 February 1997 |title=The role of organic acids in mineral weathering |journal=[[Colloids and Surfaces A: Physicochemical and Engineering Aspects]] |volume=120 |issue=1–3 |pages=167–81 |doi=10.1016/S0927-7757(96)03720-X |url=https://www.academia.edu/60332767 |access-date=19 November 2025 }}</ref> Soil organisms are hindered by high acidity, and most agricultural crops do best with mineral soils of pH&nbsp;6.5 and organic soils of pH&nbsp;5.5.{{sfn|Donahue|Miller|Shickluna|1977|pp=116–117}} Given that at low pH toxic metals (e.g. [[aluminium]], [[cadmium]], [[zinc]], [[lead]]) are positively charged as cations and organic pollutants are in non-ionic form, thus both are made more available to organisms,<ref>{{cite journal |last1=Calmano |first1=Wolfgang |last2=Hong |first2=Jihua |last3=Förstner |first3=Ulrich |date=October 1993 |title=Binding and mobilization of heavy metals in contaminated sediments affected by pH and redox potential |journal=[[Water Science and Technology]] |volume=28 |issue=8–9 |pages=223–35 |url=https://fr.1lib.sk/book/103150019/770dcc |doi=10.2166/wst.1993.0622 |bibcode=1993WSTec..28..223C |access-date=19 November 2025 }}</ref><ref>{{cite journal |last1=Ren |first1=Xiaoya |last2=Zeng |first2=Guangming |last3=Tang |first3=Lin |last4=Wang |first4=Jingjing |last5=Wan |first5=Jia |last6=Liu |first6=Yani |last7=Yu |first7=Jiangfang |last8=Yi |first8=Huan |last9=Ye |first9=Shujing |last10=Deng |first10=Rui |date=1 January 2018 |title=Sorption, transport and biodegradation: an insight into bioavailability of persistent organic pollutants in soil |journal=[[Science of the Total Environment]] |volume=610–611 |pages=1154–63 |url=http://ee.hnu.edu.cn/__local/E/E3/44/F76DCA19501AE153573A22D4C29_17709BE2_110161.pdf |doi=10.1016/j.scitotenv.2017.08.089 |pmid=28847136 |access-date=19 November 2025 |bibcode=2018ScTEn.610.1154R }}</ref> it has been suggested that plants, animals and microbes commonly living in acid soils are [[pre-adapted]] to every kind of pollution, whether of natural or human origin.<ref>{{cite journal |last=Ponge |first=Jean-François |date=July 2003 |title=Humus forms in terrestrial ecosystems: a framework to biodiversity |journal=[[Soil Biology and Biochemistry]] |volume=35 |issue=7 |pages=935–45 |url=https://www.academia.edu/20508983 |doi=10.1016/S0038-0717(03)00149-4 |bibcode=2003SBiBi..35..935P |access-date=19 November 2025 |citeseerx=10.1.1.467.4937 |s2cid=44160220 }}</ref>

In high rainfall areas, soils tend to acidify as the basic cations are forced off the soil colloids by the mass action of hydronium ions from usual or unusual [[Acid rain|rain acidity]] against those attached to the colloids. High rainfall rates can then wash the nutrients out, leaving the soil inhabited only by those organisms which are particularly efficient to uptake nutrients in very acid conditions, like in [[tropical rainforests]].<ref>{{cite journal |last=Fujii |first=Kazumichi |date=27 April 2014 |title=Soil acidification and adaptations of plants and microorganisms in Bornean tropical forests |journal=Ecological Research |volume=29 |issue=3 |pages=371–81 |doi=10.1007/s11284-014-1144-3 |doi-access=free }}</ref> Once the colloids are saturated with H<sub>3</sub>O<sup>+</sup>, the addition of any more hydronium ions or [[Aluminium hydroxide|aluminum hydroxyl]] cations drives the pH even lower (more acidic) as the soil has been left with no [[buffering capacity]].<ref>{{cite journal |last1=Kauppi |first1=Pekka |last2=Kämäri |first2=Juha |last3=Posch |first3=Maximilian |last4=Kauppi |first4=Lea |date=October 1986 |title=Acidification of forest soils: model development and application for analyzing impacts of acidic deposition in Europe |journal=[[Ecological Modelling]] |volume=33 |issue=2–4 |pages=231–53 |url=https://fr.1lib.sk/book/57310060/0ed1ea |doi=10.1016/0304-3800(86)90042-6 |bibcode=1986EcMod..33..231K |access-date=19 November 2025 }}</ref> In areas of extreme rainfall and high temperatures, clay and humus may be washed out, further reducing the buffering capacity of the soil.<ref>{{cite journal |last=Andriesse |first=Jacobus Pieter |date=May 1969 |title=A study of the environment and characteristics of tropical podzols in Sarawak (East-Malaysia) |journal=Geoderma |volume=2 |issue=3 |pages=201–27 |url=https://fr.1lib.sk/book/48380141/a3a1fd |doi=10.1016/0016-7061(69)90038-X |access-date=20 November 2025 |bibcode=1969Geode...2..201A }}</ref> In low rainfall areas, unleached calcium pushes pH to 8.5 and with the addition of exchangeable sodium, soils may reach pH&nbsp;10.<ref>{{cite journal |last=Rengasamy |first=Pichu |date=March 2006 |title=World salinization with emphasis on Australia |journal=[[Journal of Experimental Botany]] |volume=57 |issue=5 |pages=1017–23 |doi=10.1093/jxb/erj108 |pmid=16510516 |url=https://www.researchgate.net/publication/7266400 |access-date=20 November 2025 }}</ref> Beyond a pH of 9, plant growth is reduced.<ref>{{cite journal |last1=Arnon |first1=Daniel I. |last2=Johnson |first2=Clarence M. |date=October 1942 |title=Influence of hydrogen ion concentration on the growth of higher plants under controlled conditions |journal=[[Plant Physiology (journal)|Plant Physiology]] |volume=17 |issue=4 |pages=525–39 |doi=10.1104/pp.17.4.525 |pmid=16653803 |pmc=438054 |doi-access=free }}</ref> High pH results in low [[micro-nutrient]] mobility, but water-soluble [[chelates]] of those nutrients can correct the deficit.<ref>{{cite journal |last1=Chaney |first1=Rufus L. |last2=Brown |first2=John C. |last3=Tiffin |first3=Lee O. |date=October 1972 |title=Obligatory reduction of ferric chelates in iron uptake by soybeans |journal=[[Plant Physiology (journal)|Plant Physiology]] |volume=50 |issue=2 |pages=208–13 |doi=10.1104/pp.50.2.208 |pmid=16658143 |pmc=366111 |doi-access=free }}</ref> [[Sodium]] can be reduced by the addition of [[gypsum]] ([[Calcium sulfate|calcium sulphate]]) as calcium adheres to clay more tightly than does sodium causing sodium to be pushed into the soil water solution where it can be washed out by an abundance of water.{{sfn|Donahue|Miller|Shickluna|1977|pp=116–119}}<ref>{{cite journal |last1=Ahmad |first1=Sagheer |last2=Ghafoor |first2=Abdul |last3=Qadir |first3=Manzoor |last4=Aziz |first4=M. Abbas |year=2006 |title=Amelioration of a calcareous saline-sodic soil by gypsum application and different crop rotations |journal=International Journal of Agriculture and Biology |volume=8 |issue=2 |pages=142–6 |url=https://www.researchgate.net/publication/228966353 |access-date=20 November 2025 }}</ref>

==== Base saturation percentage ====

There are acid-forming cations (e.g. hydronium, aluminium, iron) and there are base-forming cations (e.g. calcium, magnesium, sodium). The fraction of the negatively-charged soil colloid exchange sites (CEC) that are occupied by base-forming cations is called [[base saturation]]. If a soil has a CEC of 20&nbsp;meq and 5&nbsp;meq are aluminium and hydronium cations (acid-forming), the remainder of positions on the colloids ({{nowrap|1=20 − 5 = 15 meq}}) are assumed occupied by base-forming cations, so that the base saturation is {{nowrap|1=15 ÷ 20 × 100% = 75%}} (the compliment 25% is assumed acid-forming cations). Base saturation is almost in direct proportion to pH (it increases with increasing pH).<ref>{{cite journal |last1=McFee |first1=William W. |last2=Kelly |first2=J. Michael |last3=Beck |first3=Robert H. |date=March 1977 |title=Acid precipitation effects on soil pH and base saturation of exchange sites |journal=[[Water, Air, & Soil Pollution|Water, Air, and Soil Pollution]] |volume=7 |issue=3 |pages=401–8 |doi=10.1007/BF00284134 |bibcode=1977WASP....7..401M |url=https://www.researchgate.net/publication/226736129 |access-date=20 November 2025 }}</ref> It is of use in calculating the amount of lime needed to neutralise an acid soil (lime requirement). The amount of lime needed to neutralize a soil must take account of the amount of acid forming ions on the colloids (exchangeable acidity), not just those in the soil water solution (free acidity).<ref>{{cite journal |last1=Farina |first1=Martin Patrick W. |last2=Sumner |first2=Malcolm E. |last3=Plank |first3=C. Owen |last4=Letzsch |first4=W. Stephen |date=1 September 1980 |title=Exchangeable aluminum and pH as indicators of lime requirement for corn |journal=[[Soil Science Society of America Journal]] |volume=44 |issue=5 |pages=1036–41 |url=https://www.researchgate.net/publication/250123873 |access-date=20 November 2025 |doi=10.2136/sssaj1980.03615995004400050033x |bibcode=1980SSASJ..44.1036F }}</ref> The addition of enough lime to neutralize the soil water solution will be insufficient to change the pH, as the acid forming cations stored on the soil colloids will tend to restore the original pH condition as they are pushed off those colloids by the calcium of the added lime.{{sfn|Donahue|Miller|Shickluna|1977|pp=119–120}}

====Buffering====
{{Further|Soil conditioner}}
The resistance of soil to change in pH, as a result of the addition of acid or basic material, is a measure of the [[buffering capacity]] of a soil and (for a particular soil type) increases as the [[Cation-exchange capacity|CEC]] increases. Hence, pure sand has almost no buffering ability, though soils high in [[colloid]]s (whether mineral or organic) have high buffering capacity.<ref>{{cite journal |last1=Sposito |first1=Garrison |last2=Skipper |first2=Neal T. |last3=Sutton |first3=Rebecca |last4=Park |first4=Sun-Ho |last5=Soper |first5=Alan K. |last6=Greathouse |first6=Jeffery A. |date=30 March 1999 |title=Surface geochemistry of the clay minerals |journal=[[Proceedings of the National Academy of Sciences of the United States of America]] |volume=96 |issue=7 |pages=3358–64 |doi=10.1073/pnas.96.7.3358 |pmid=10097044 |pmc=34275 |bibcode=1999PNAS...96.3358S |doi-access=free }}</ref> Buffering occurs by cation exchange and [[Neutralization (chemistry)|neutralisation]]. However, colloids are not the only regulators of soil pH. The role of [[carbonates]] should be underlined, too.<ref>{{cite journal |last=Bache |first=Bryon W. |date=August 1984 |title=The role of calcium in buffering soils |journal=[[Plant, Cell & Environment]] |volume=7 |issue=6 |pages=391–5 |doi=10.1111/j.1365-3040.1984.tb01428.x |url=https://fr.1lib.sk/book/41305037/97f430 |access-date=20 November 2025 }}</ref> More generally, according to pH levels, several buffer systems take precedence over each other, from [[calcium carbonate]] [[buffer range]] to iron buffer range.<ref>{{cite book |last=Ulrich |first=Bernhard |title=Effects of accumulation of air pollutants in forest ecosystems |chapter=Soil acidity and its relations to acid deposition |date=1983 |chapter-url=https://archive.org/details/ulrich-1983 |pages=127–46 |edition=1st |editor-last1=Ulrich |editor-first1=Bernhard |editor-last2=Pankrath |editor-first2=Jürgen |publisher=[[D. Reidel Publishing Company]] |location=Dordrecht, The Netherlands |isbn=978-94-009-6985-8 |doi=10.1007/978-94-009-6983-4_10 |access-date=20 November 2025 }}</ref>

=== Redox ===
{{main|Redox#Redox_reactions_in_soils}}
{{See also|Table of standard reduction potentials for half-reactions important in biochemistry}}

Soil chemical reactions involve some combination of proton and [[electron transfer]]. [[Redox|Oxidation]] occurs if there is a loss of electrons in the transfer process while [[Redox|reduction]] occurs if there is a gain of electrons. [[Reduction potential]] is measured in volts or millivolts. Soil microbial communities develop along [[electron transport chain]]s, forming electrically conductive [[Geobacter#Biofilm conductivity|biofilms]], and developing networks of [[bacterial nanowires]].

Redox factors act on soil development, with [[redoximorphic features|redoximorphic color features]] providing critical information for soil interpretation. Understanding the [[Redox gradient#Terrestrial Environments|redox gradient]] is important to managing [[carbon sequestration]], [[bioremediation]], [[Pedosphere#Redox conditions in wetland soils|wetland delineation]], and [[soil-based microbial fuel cell]]s.

==Nutrients==
{| class="wikitable sortable floatright" 
|+ Plant nutrients, their chemical symbols, and the ionic forms common in soils and available for plant uptake{{sfn|Donahue|Miller|Shickluna|1977|p=125}}
|-
! Element !! Symbol !! Ion or molecule
|-
| Carbon || C || CO<sub>2</sub> (mostly through leaves)
|-
| Hydrogen || H || H<sup>+</sup>, H<sub>2</sub>O (water)
|-
| Oxygen || O || O<sup>2−</sup>, OH<sup>−</sup>, {{chem|CO|3|2−}}, {{chem|SO|4|2−}}, CO<sub>2</sub>
|-
| Phosphorus || P || {{chem|H|2|PO|4|−}}, {{chem|HPO|4|2−}} (phosphates)
|-
| Potassium || K || K<sup>+</sup>
|-
| Nitrogen || N || {{chem|NH|4|+}}, {{chem|NO|3|−}} (ammonium, nitrate)
|-
| Sulfur || S || {{chem|SO|4|2−}}
|-
| Calcium || Ca || Ca<sup>2+</sup>
|-
| Iron || Fe || Fe<sup>2+</sup>, Fe<sup>3+</sup> (ferrous, ferric)
|-
| Magnesium || Mg || Mg<sup>2+</sup>
|-
| Boron || B || H<sub>3</sub>BO<sub>3</sub>, {{chem|H|2|BO|3|−}}, {{chem|B(OH)|4|−}}
|-
| Manganese || Mn || Mn<sup>2+</sup>
|-
| Copper || Cu || Cu<sup>2+</sup>
|-
| Zinc || Zn || Zn<sup>2+</sup>
|-
| Molybdenum || Mo || {{chem|MoO|4|2−}} (molybdate)
|-
| Chlorine || Cl || Cl<sup>−</sup> (chloride)
|}
{{Main|Plant nutrients in soil|Plant nutrition|Soil pH#Effect of soil pH on plant growth}}
Seventeen elements or nutrients are essential for plant growth and reproduction. They are [[carbon]] (C), [[hydrogen]] (H), [[oxygen]] (O), [[nitrogen]] (N), [[phosphorus]] (P), [[potassium]] (K), [[sulfur]] (S), [[calcium]] (Ca), [[magnesium]] (Mg), [[iron]] (Fe), [[boron]] (B), manganese (Mn), [[copper]] (Cu), [[zinc]] (Zn), [[molybdenum]] (Mo), [[nickel]] (Ni) and [[chlorine]] (Cl).{{sfn|Dean|1957|p=80}}{{sfn|Russel|1957|pp=123–125}}<ref name=Brady1984>{{cite book |title=The nature and properties of soils |year=1984 |edition=9th |last=Brady |first=Nyle C. |publisher=[[Macmillan Publishing Company]] |location=New York, New York |url=https://fr.1lib.sk/book/12005464/452990 |access-date=16 March 2025 |isbn=978-0-02-946030-6 }}</ref> Nutrients required for plants to complete their life cycle are considered [[essential nutrients]]. Nutrients that enhance the growth of plants but are not necessary to complete the plant's life cycle are considered non-essential. Except for carbon, hydrogen, and oxygen, which are supplied by carbon dioxide and water, and nitrogen, provided through nitrogen fixation,<ref name=Brady1984/> the nutrients derive originally from the mineral component of the soil. The [[law of the minimum]] expresses that when the available form of a nutrient is not in enough proportion in the soil solution, other nutrients cannot be taken up at an optimum rate by a plant.<ref>{{cite journal |last1=Van der Ploeg |first1=Rienk R. |last2=Böhm |first2=Wolfgang |last3=Kirkham |first3=Mary Beth |year=1999 |title=On the origin of the theory of mineral nutrition of plants and the Law of the Minimum |journal=[[Soil Science Society of America Journal]] |volume=63 |issue=5 |pages=1055–62 |doi=10.2136/sssaj1999.6351055x |citeseerx=10.1.1.475.7392 |bibcode=1999SSASJ..63.1055V |doi-access=free }}</ref> A particular nutrient ratio of the soil solution is thus mandatory for optimizing plant growth, a value which might differ from nutrient ratios calculated from plant composition.<ref>{{cite journal |last1=Knecht |first1=Magnus F. |last2=Göransson |first2=Anders |year=2004 |title=Terrestrial plants require nutrients in similar proportions |journal=Tree Physiology |volume=24 |issue=4 |pages=447–60 |doi=10.1093/treephys/24.4.447 |pmid=14757584 |url=https://fr.1lib.sk/book/72174734/946166 |access-date=16 March 2025 }}</ref>

Plant uptake of nutrients can only proceed when present in a plant-available form. In most situations, nutrients are absorbed in an [[Ionic compound|ionic]] form from (or together with) soil water. Although minerals are the origin of most nutrients, and the bulk of most nutrient elements in the soil is held in crystalline form within [[Primary mineral|primary]] and [[secondary mineral]]s, they weather too slowly to support rapid plant growth. For example, the application of finely ground minerals, [[feldspar]] and [[apatite]], to soil seldom provides the necessary amounts of potassium and phosphorus at a rate sufficient for good plant growth, as most of the nutrients remain bound in the crystals of those minerals.{{sfn|Dean|1957|pp=80–81}} However, plants are able to stimulate [[mineral weathering]], and thus the availability of mineral-bound nutrients, through various processes, both direct (e.g. weathering agents, [[biogenic minerals]]) and indirect (e.g. [[mycorrhizal fungi]], [[rhizosphere]] bacteria).<ref>{{cite journal |last1=Kelly |first1=Eugene F. |last2=Chadwick |first2=Oliver A. |last3=Hiinski |first3=Thomas E. |year=1998 |title=The effect of plants on mineral weathering |journal=Biogeochemistry |volume=42 |issue=1–2 |pages=21–53 |doi=10.1023/A:1005919306687 |bibcode=1998Biogc..42...21K |url=https://www.academia.edu/87628533 |access-date=23 March 2025 }}</ref><ref>{{cite journal |last1=Calvaruso |first1=Christophe |last2=Turpault |first2=Marie-Pierre |last3=Frey-Klett |first3=Pascale |date=February 2006 |title=Root-associated bacteria contribute to mineral weathering and to mineral nutrition in trees: a budgeting analysis |journal=[[Applied and Environmental Microbiology]] |volume=72 |issue=2 |pages=1258–66 |doi=10.1128/AEM.72.2.1258-1266.2006 |pmid=16461674 |pmc=1392890 |bibcode=2006ApEnM..72.1258C }}</ref><ref>{{cite journal |last1=Van Schöll |first1=Laura |last2=Kuyper |first2=Thomas W. |last3=Smits |first3=Mark M. |last4=Landeweert |first4=Renske |last5=Hoffland |first5=Ellis |last6=Van Breemen |first6=Nico |date=21 December 2007 |title=Rock-eating mycorrhizas: their role in plant nutrition and biogeochemical cycles |journal=[[Plant and Soil]] |volume=303 |issue=1–2 |pages=35–47 |doi=10.1007/s11104-007-9513-0 |url=https://core.ac.uk/download/pdf/29259822.pdf |access-date=23 March 2025 }}</ref>

The nutrients adsorbed onto the surfaces of clay colloids and soil organic matter provide a more accessible reservoir of many plant nutrients (e.g., K, Ca, Mg, P, Zn). As plants absorb the nutrients from the soil water, the soluble pool is replenished from the surface-bound pool. The decomposition of soil organic matter by microorganisms is another mechanism whereby the soluble pool of nutrients is replenished – this is important for the supply of plant-available N, S, P, and B from soil.<ref name="Roy2006Chapter4">{{cite book |chapter-url=https://www.fao.org/fileadmin/templates/soilbiodiversity/Downloadable_files/fpnb16.pdf#page=61.14 |title=Plant nutrition for food security: a guide for integrated nutrient management |last1=Roy |first1=R. N. |last2=Finck |first2=Arnold |last3=Blair |first3=Graeme J. |last4=Tandon |first4=Hari Lal Singh |publisher=[[Food and Agriculture Organization of the United Nations]] |year=2006 |isbn=978-92-5-105490-1 |location=Rome, Italy |pages=43–90 |chapter=Soil fertility and crop production |access-date=30 March 2025 }}</ref>

Gram for gram, the capacity of [[humus]] to hold nutrients and water is far greater than that of clay minerals, most of the soil [[Cation-exchange capacity|cation exchange capacity]] arising from charged [[carboxylic]] groups on organic matter.<ref>{{cite journal |last1=Parfitt |first1=Roger L. |last2=Giltrap |first2=Donna J. |last3=Whitton |first3=Joe S. |year=1995 |title=Contribution of organic matter and clay minerals to the cation exchange capacity of soil |journal=Communications in Soil Science and Plant Analysis |volume=26 |issue=9–10 |pages=1343–55 |url=https://www.researchgate.net/publication/249073571 |doi=10.1080/00103629509369376 |bibcode=1995CSSPA..26.1343P |access-date=30 March 2025 }}</ref> However, despite the remarkable capacity of humus to retain water once water-soaked, its high [[hydrophobicity]] decreases its [[wettability]] once dry.<ref>{{cite journal |last1=Hajnos |first1=Mieczyslaw |last2=Jozefaciuk |first2=Grzegorz |last3=Sokołowska |first3=Zofia |last4=Greiffenhagen |first4=Andreas |last5=Wessolek |first5=Gerd |year=2003 |title=Water storage, surface, and structural properties of sandy forest humus horizons |journal=Journal of Plant Nutrition and Soil Science |volume=166 |issue=5 |pages=625–34 |url=https://www.researchgate.net/publication/229970348 |doi=10.1002/jpln.200321161 |bibcode=2003JPNSS.166..625H |access-date=30 March 2025 }}</ref> Small amounts of humus may remarkably increase the soil's capacity to promote plant growth.{{sfn|Donahue|Miller|Shickluna|1977|pp=123–131}}<ref name="Roy2006Chapter4"/>

==Soil organic matter==
{{main|Soil organic matter}}{{Overly detailed|section|details=details could be moved into main article|date=April 2021}}
The organic material in soil is made up of [[organic compounds]] and includes plant, animal and microbial material, both living and dead. A typical soil has a biomass composition of 70% microorganisms, 22% macrofauna, and 8% roots. The living component of an acre of soil may include 900&nbsp;lb of earthworms, 2400&nbsp;lb of fungi, 1500&nbsp;lb of bacteria, 133&nbsp;lb of protozoa and 890&nbsp;lb of arthropods and algae.<ref>{{cite journal |last1=Pimentel |first1=David |last2=Harvey |first2=Celia |last3=Resosudarmo |first3=Pradnja |last4=Sinclair |first4=K. |last5=Kurz |first5=D. |last6=McNair |first6=M. |last7=Crist |first7=S. |last8=Shpritz |first8=L. |last9=Fitton |first9=L. |last10=Saffouri |first10=R. |last11=Blair |first11=R. |year=1995 |title=Environmental and economic costs of soil erosion and conservation benefits |journal=[[Science (journal)|Science]] |volume=267 |issue=5201 |pages=1117–23 |url=https://www.academia.edu/9512072 |doi=10.1126/science.267.5201.1117 |pmid=17789193 |bibcode=1995Sci...267.1117P |s2cid=11936877 |access-date=6 April 2025 |archive-url=https://web.archive.org/web/20161213065558/http://www.rachel.org/files/document/Environmental_and_Economic_Costs_of_Soil_Erosi.pdf |archive-date=13 December 2016 |url-status=live }}</ref>

A few percent of the soil organic matter, with small [[residence time]], consists of the microbial [[biomass]] and [[metabolites]] of bacteria, [[mold]]s, and [[Actinomycetia|actinomycete]]s that work to break down the dead organic matter.<ref>{{cite journal |last1=Schnürer |first1=Johan |last2=Clarholm |first2=Marianne |last3=Rosswall |first3=Thomas |year=1985 |title=Microbial biomass and activity in an agricultural soil with different organic matter contents |journal=[[Soil Biology and Biochemistry]] |volume=17 |issue=5 |pages=611–18 |url=https://www.academia.edu/20647751 |doi=10.1016/0038-0717(85)90036-7 |bibcode=1985SBiBi..17..611S |access-date=6 April 2025 }}</ref><ref>{{cite journal |last=Sparling |first=Graham P. |year=1992 |title=Ratio of microbial biomass carbon to soil organic carbon as a sensitive indicator of changes in soil organic matter |journal=[[Australian Journal of Soil Research]] |volume=30 |issue=2 |pages=195–207 |url=https://www.researchgate.net/publication/248884528 |doi=10.1071/SR9920195 |bibcode=1992SoilR..30..195S |access-date=6 April 2025 }}</ref> Were it not for the action of these micro-organisms, the entire carbon dioxide part of the atmosphere would be sequestered as organic matter in the soil. However, in the same time soil microbes contribute to [[carbon sequestration]] in the topsoil through the formation of stable humus.<ref>{{cite journal |last1=Varadachari |first1=Chandrika |last2=Ghosh |first2=Kunal |year=1984 |title=On humus formation |journal=[[Plant and Soil]] |volume=77 |issue=2 |pages=305–13 |doi=10.1007/BF02182933 |bibcode=1984PlSoi..77..305V |s2cid=45102095 |url=https://www.researchgate.net/publication/225528442 |access-date=6 April 2025 }}</ref> In the aim to sequester more carbon in the soil for alleviating the [[greenhouse effect]] it would be more efficient in the long-term to stimulate [[humification]] than to decrease litter [[decomposition]].<ref>{{cite journal |last=Prescott |first=Cindy E. |year=2010 |title=Litter decomposition: what controls it and how can we alter it to sequester more carbon in forest soils? |journal=Biogeochemistry |volume=101 |issue=1 |pages=133–49 |doi=10.1007/s10533-010-9439-0 |bibcode=2010Biogc.101..133P |s2cid=93834812 |url=https://www.researchgate.net/publication/226936910 |access-date=6 April 2025 }}</ref>

The main part of soil organic matter is a complex assemblage of small organic molecules, collectively called [[humus]] or [[humic]] substances. The use of these terms, which do not rely on a clear chemical classification, has been considered as obsolete.<ref>{{cite journal |last1=Lehmann |first1=Johannes |last2=Kleber |first2=Markus |year=2015 |title=The contentious nature of soil organic matter |journal=[[Nature (journal)|Nature]] |volume=528 |issue=7580 |pages=60–68 |url=https://www.css.cornell.edu/faculty/lehmann/publ/Nature%20528,%2060-68,%202015%20Lehmann.pdf |doi=10.1038/nature16069 |pmid=26595271 |bibcode=2015Natur.528...60L |s2cid=205246638 |access-date=13 April 2025 }}</ref> Other studies showed that the classical notion of molecule is not convenient for humus, which escaped most attempts done over two centuries to resolve it in unit components, but still is chemically distinct from polysaccharides, lignins and proteins.<ref name="Piccolo2002">{{cite journal |last=Piccolo |first=Alessandro |year=2002 |title=The supramolecular structure of humic substances: a novel understanding of humus chemistry and implications in soil science |journal=Advances in Agronomy |volume=75 |pages=57–134 |url=https://www.researchgate.net/publication/222526145 |doi=10.1016/S0065-2113(02)75003-7 |isbn=978-0-12-000793-6 |access-date=13 April 2025 }}</ref>

Most living things in soils, including plants, animals, bacteria, and fungi, are dependent on organic matter for nutrients and/or energy. Soils have organic compounds in varying degrees of decomposition, the rate of which is dependent on the temperature, soil moisture, and aeration. Bacteria and fungi feed on the raw organic matter, which are fed upon by [[protozoa]], which in turn are fed upon by [[nematodes]], [[annelids]] and [[arthropod]]s, themselves able to consume and transform raw or humified organic matter. This has been called the [[soil food web]], through which all organic matter is processed as in a [[digestive system]].<ref>{{cite journal |last=Scheu |first=Stefan |year=2002 |title=The soil food web: structure and perspectives |journal=European Journal of Soil Biology |volume=38 |issue=1 |pages=11–20 |url=https://www.researchgate.net/publication/263041521 |doi=10.1016/S1164-5563(01)01117-7 |bibcode=2002EJSB...38...11S |access-date=13 April 2025 }}</ref> Organic matter holds soils open, allowing the infiltration of air and water, and may hold as much as twice its weight in water. Many soils, including desert and rocky-gravel soils, have little or no organic matter. Soils that are all organic matter, such as [[peat]] ([[histosols]]), are infertile.<ref name=Foth1984>{{Cite book |last=Foth |first=Henry D. |year=1984 |title=Fundamentals of soil science |edition=8th |page=139 |url=http://base.dnsgb.com.ua/files/book/Agriculture/Soil/Fundamentals-of-Soil-Science.pdf |isbn=978-0-471-52279-9 |publisher=Wiley |location=New York, New York |access-date=13 April 2025 |archive-date=12 November 2020 |archive-url=https://web.archive.org/web/20201112034423/http://base.dnsgb.com.ua/files/book/Agriculture/Soil/Fundamentals-of-Soil-Science.pdf |url-status=live }}</ref> In its earliest stage of decomposition, the original organic material is often called raw organic matter. The final stage of decomposition is called humus.

In [[grassland]], much of the organic matter added to the soil is from the deep, fibrous, grass root systems. By contrast, tree leaves falling on the forest floor are the principal source of soil organic matter in the forest. Another difference is the frequent occurrence in the grasslands of fires that destroy large amounts of aboveground material but stimulate even greater contributions from roots. Also, the much greater acidity under any forests inhibits the action of certain soil organisms that otherwise would mix much of the surface litter into the mineral soil. As a result, the soils under grasslands generally develop a thicker [[A horizon]] with a deeper distribution of organic matter than in comparable soils under forests, which characteristically store most of their organic matter in the forest floor ([[O horizon]]) and thin A horizon.<ref name="Ponge2003">{{cite journal |last=Ponge |first=Jean-François |year=2003 |title=Humus forms in terrestrial ecosystems: a framework to biodiversity |journal=[[Soil Biology and Biochemistry]] |volume=35 |issue=7 |pages=935–45 |doi=10.1016/S0038-0717(03)00149-4 |bibcode=2003SBiBi..35..935P |url=https://www.academia.edu/45579598 |url-status=live |archive-url=https://web.archive.org/web/20160129153903/https://www.researchgate.net/publication/222567430 |archive-date=29 January 2016 |citeseerx=10.1.1.467.4937 |s2cid=44160220 |access-date=13 April 2025 }}</ref>

===Humus===
Humus refers to organic matter that has been decomposed by soil microflora and fauna to the point where it is resistant to further breakdown.<ref name="Ponge2022">{{cite journal |last=Ponge |first=Jean-François |date=August 2022 |title=Humus: dark side of life or intractable "aether"? |journal=Pedosphere |volume=32 |issue=4 |pages=660–64 |url=https://www.researchgate.net/publication/360175852 |doi=10.1016/S1002-0160(21)60013-9 |bibcode=2022Pedos..32..660P |access-date=13 April 2025 }}</ref> Humus usually constitutes only five percent of the soil or less by volume, but it is an essential source of nutrients and adds important textural qualities crucial to [[soil health]] and plant growth.<ref>{{cite web |url=https://humates.com/wp-content/uploads/2020/04/ORGANICMATTERPettit.pdf |last=Pettit |first=Robert E. |title=Organic matter, humus, humate, humic acid, fulvic acid and humin: their importance in soil fertility and plant health |access-date=13 April 2025 }}</ref> Humus also feeds arthropods, [[termite]]s and [[earthworm]]s which further improve the soil.<ref>{{cite journal |last1=Ji |first1=Rong |last2=Kappler |first2=Andreas |last3=Brune |first3=Andreas |year=2000 |title=Transformation and mineralization of synthetic <sup>14</sup>C-labeled humic model compounds by soil-feeding termites |journal=[[Soil Biology and Biochemistry]] |volume=32 |issue=8–9 |pages=1281–91 |doi=10.1016/S0038-0717(00)00046-8 |citeseerx=10.1.1.476.9400 |url=https://www.academia.edu/13008941 |access-date=20 April 2025 }}</ref> The end product, humus, is suspended in [[colloidal]] form in the soil solution and forms a [[weak acid]] that can attack silicate minerals by [[Chelation|chelating]] their iron and aluminum atoms.<ref>{{cite book |last1=Drever |first1=James I. |last2=Vance |first2=George F. |title=Organic acids in geological processes |chapter=Role of soil organic acids in mineral weathering processes |year=1994 |doi=10.1007/978-3-642-78356-2_6 |editor-last1=Pittman |editor-first1=Edward D. |editor-last2=Lewan |editor-first2=Michael D. |publisher=[[Springer Science+Business Media|Springer]] |location=Berlin, Germany |pages=138–61 |isbn=978-3-642-78356-2 |chapter-url=https://fr.1lib.sk/book/53559896/96a34d |access-date=20 April 2025 }}</ref> Humus has a high cation and anion exchange capacity that on a dry weight basis is many times greater than that of clay colloids. It also acts as a buffer, like clay, against changes in pH and soil moisture.<ref name="Piccolo1996">{{cite book |last=Piccolo |first=Alessandro |year=1996 |chapter=Humus and soil conservation |doi=10.1016/B978-044481516-3/50006-2 |title=Humic substances in terrestrial ecosystems |editor-first=Alessandro |editor-last=Piccolo |publisher= [[Elsevier]] |location=Amsterdam, the Netherlands |pages=225–264 |isbn=978-0-444-81516-3 |chapter-url=https://www.researchgate.net/publication/281451183 |access-date=20 April 2025 }}</ref>

[[Humic acid]]s and [[fulvic acid]]s, which begin as raw organic matter, are important constituents of humus. After the death of plants, animals, and microbes, microbes begin to feed on the residues through their production of extra-cellular soil enzymes, resulting finally in the formation of humus.<ref>{{cite journal |last1=Varadachari |first1=Chandrika |last2=Ghosh |first2=Kunal |year=1984 |title=On humus formation |journal=[[Plant and Soil]] |volume=77 |issue=2 |pages=305–13 |url=https://www.researchgate.net/publication/225528442 |doi=10.1007/BF02182933 |bibcode=1984PlSoi..77..305V |s2cid=45102095 |access-date=20 April 2025 }}</ref> As the residues break down, only molecules made of [[aliphatic compound|aliphatic]] and [[aromatic hydrocarbon|aromatic]] hydrocarbons, assembled and stabilized by oxygen and [[hydrogen bond]]s, remain in the form of complex molecular assemblages collectively called humus.<ref name="Piccolo2002"/> Humus is never pure in the soil, because it reacts with metals and clays to form complexes which further contribute to its stability and to soil structure.<ref name="Piccolo1996"/> Although the structure of humus has in itself few nutrients (with the exception of constitutive metals such as calcium, iron and aluminum) it is able to attract and link, by weak bonds, cation and anion nutrients that can further be released into the soil solution in response to selective root uptake and changes in soil pH, a process of paramount importance for the maintenance of fertility in tropical soils.<ref>{{cite journal |last1=Mendonça |first1=Eduardo S. |last2=Rowell |first2=David L. |year=1996 |title=Mineral and organic fractions of two oxisols and their influence on effective cation-exchange capacity |journal=[[Soil Science Society of America Journal]] |volume=60 |issue=6 |pages=1888–92 |url=https://fr.1lib.sk/book/55342950/7121f7 |doi=10.2136/sssaj1996.03615995006000060038x |bibcode=1996SSASJ..60.1888M |access-date=20 April 2025 }}</ref>

[[Lignin]] is resistant to breakdown and accumulates within the soil. It also reacts with [[proteins]],<ref>{{cite journal |last1=Heck |first1=Tobias |last2=Faccio |first2=Greta |last3=Richter |first3=Michael |last4=Thöny-Meyer |first4=Linda |year=2013 |title=Enzyme-catalyzed protein crosslinking |journal=[[Applied Microbiology and Biotechnology]] |volume=97 |issue=2 |pages=461–75 |url=https://www.researchgate.net/publication/233769618 |doi=10.1007/s00253-012-4569-z |pmid=23179622 |pmc=3546294 |access-date=27 April 2025 }}</ref> which further increases its resistance to decomposition, including enzymatic decomposition by microbes.<ref>{{cite journal |last1=Lynch |first1=D. L. |last2=Lynch |first2=C. C. |year=1958 |title=Resistance of protein–lignin complexes, lignins and humic acids to microbial attack |journal=[[Nature (journal)|Nature]] |volume=181 |issue=4621 |pages=1478–79 |url=https://fr.1lib.sk/book/42467876/142898 |doi=10.1038/1811478a0 |pmid=13552710 |bibcode=1958Natur.181.1478L |s2cid=4193782 |access-date=27 April 2025 }}</ref> [[Fat]]s and [[wax]]es from plant matter have still more resistance to decomposition and persist in soils for thousand years, hence their use as tracers of past vegetation in buried soil layers.<ref>{{cite journal |last1=Dawson |first1=Lorna A. |last2=Hillier |first2=Stephen |year=2010 |title=Measurement of soil characteristics for forensic applications |journal=[[Surface and Interface Analysis]] |volume=42 |issue=5 |pages=363–77 |url=https://www.academia.edu/128162468 |doi=10.1002/sia.3315 |s2cid=54213404 |access-date=27 April 2025 |archive-date=8 May 2021 |archive-url=https://web.archive.org/web/20210508065204/https://people.ok.ubc.ca/robrien/soil%20characteristics.pdf |url-status=live }}</ref> Clay soils often have higher organic contents that persist longer than soils without clay as the organic molecules adhere to and are stabilised by the clay.<ref>{{cite journal |last1=Manjaiah |first1=Kanchikeri Math |last2=Kumar |first2=Sarvendra |last3=Sachdev |first3=M. S. |last4=Sachdev |first4=P. |last5=Datta |first5=Samar Chandra |year=2010 |title=Study of clay–organic complexes |journal=[[Current Science]] |volume=98 |issue=7 |pages=915–21 |url=https://www.researchgate.net/publication/228867334 |access-date=27 April 2025 }}</ref> Proteins normally decompose readily, to the exception of [[scleroproteins]], but when bound to clay particles they become more resistant to decomposition.<ref>{{cite journal |last=Theng |first=Benny K.G. |year=1982 |title=Clay-polymer interactions: summary and perspectives |journal=Clays and Clay Minerals |volume=30 |issue=1 |pages=1–10 |doi=10.1346/CCMN.1982.0300101 |bibcode=1982CCM....30....1T |citeseerx=10.1.1.608.2942 |s2cid=98176725 |url=https://www.researchgate.net/publication/238684938 |access-date=27 April 2025 }}</ref> As for other proteins clay particles absorb the enzymes exuded by microbes, decreasing [[enzyme activity]] while protecting [[extracellular enzymes]] from degradation.<ref>{{cite journal |last1=Tietjen |first1=Todd |last2=Wetzel |first2=Robert G. |year=2003 |title=Extracellular enzyme-clay mineral complexes: enzyme adsorption, alteration of enzyme activity, and protection from photodegradation |journal=Aquatic Ecology |volume=37 |issue=4 |pages=331–39 |doi=10.1023/B:AECO.0000007044.52801.6b |bibcode=2003AqEco..37..331T |s2cid=6930871 |url=https://www.vliz.be/imisdocs/publications/ocrd/54440.pdf |access-date=24 April 2025 }}</ref> The addition of organic matter to clay soils can render that organic matter and any added nutrients inaccessible to plants and microbes for many years.<ref>{{cite journal |last1=Tahir |first1=Shermeen |last2=Marschner |first2=Petra |year=2017 |title=Clay addition to sandy soil: influence of clay type and size on nutrient availability in sandy soils amended with residues differing in C/N ratio |journal=[[Pedosphere]] |volume=27 |issue=2 |pages=293–305 |url=https://www.researchgate.net/publication/314221508 |doi=10.1016/S1002-0160(17)60317-5 |bibcode=2017Pedos..27..293T |access-date=24 April 2025 }}</ref> A study showed increased soil fertility following the addition of mature compost to a clay soil.<ref>{{cite journal |last1=Melero |first1=Sebastiana |last2=Madejón |first2=Engracia |last3=Ruiz |first3=Juan Carlos |last4=Herencia |first4=Juan Francisco |year=2007 |title=Chemical and biochemical properties of a clay soil under dryland agriculture system as affected by organic fertilization |journal=European Journal of Agronomy |volume=26 |issue=3 |pages=327–34 |url=https://fr.1lib.sk/book/45675038/0dbbc0 |doi=10.1016/j.eja.2006.11.004 |bibcode=2007EuJAg..26..327M |access-date=24 April 2025 }}</ref> High soil [[tannin]] content can cause nitrogen to be sequestered as resistant tannin-protein complexes.<ref>{{cite journal |last1=Joanisse |first1=Gilles D. |last2=Bradley |first2=Robert L. |last3=Preston |first3=Caroline M. |last4=Bending |first4=Gary D. |title=Sequestration of soil nitrogen as tannin–protein complexes may improve the competitive ability of sheep laurel (Kalmia angustifolia) relative to black spruce (Picea mariana) |journal=[[New Phytologist]] |year=2009 |volume=181 |pages=187–98 |doi=10.1111/j.1469-8137.2008.02622.x |issue=1 |pmid=18811620 |doi-access=free |bibcode=2009NewPh.181..187J }}</ref><ref name=Fierer2001>{{cite journal |last1=Fierer |first1=Noah |last2=Schimel |first2=Joshua P. |last3=Cates |first3=Rex G. |last4=Zou |first4=Jiping |title=Influence of balsam poplar tannin fractions on carbon and nitrogen dynamics in Alaskan taiga floodplain soils |journal=[[Soil Biology and Biochemistry]] |year=2001 |volume=33 |pages=1827–39 |doi=10.1016/S0038-0717(01)00111-0 |issue=12–13 |bibcode=2001SBiBi..33.1827F |url=https://www.academia.edu/12814037 |access-date=24 April 2025 }}</ref>

Humus formation is a process dependent on the amount of plant material added each year and the type of base soil. Both are affected by climate and the type of organisms present.<ref name="Ponge2003"/> Soils with humus can vary in nitrogen content but typically have 3 to 6&nbsp;percent nitrogen. Raw organic matter, as a reserve of nitrogen and phosphorus, is a vital component affecting [[Fertile soil|soil fertility]].<ref name="Foth1984"/> Humus also absorbs water, and expands and shrinks between dry and wet states to a higher extent than clay, increasing soil porosity.<ref>{{cite journal |last1=Peng |first1=Xinhua |last2=Horn |first2=Rainer |title=Anisotropic shrinkage and swelling of some organic and inorganic soils |journal=European Journal of Soil Science |year=2007 |volume=58 |issue=1 |pages=98–107 |doi=10.1111/j.1365-2389.2006.00808.x |bibcode=2007EuJSS..58...98P |url=https://www.academia.edu/56639603 |access-date=4 May 2025 }}</ref> Humus is less stable than the soil's mineral constituents, as it is reduced by microbial [[decomposition]], and over time its concentration diminishes without the addition of new organic matter. However, humus in its most stable forms may persist over centuries if not millennia.<ref>{{cite journal |last1=Wang |first1=Yang |last2=Amundson |first2=Ronald |last3=Trumbmore |first3=Susan |title=Radiocarbon dating of soil organic matter |journal=[[Quaternary Research]] |year=1996 |volume=45 |issue=3 |pages=282–88 |doi=10.1006/qres.1996.0029 |bibcode=1996QuRes..45..282W |s2cid=73640995 |url=https://escholarship.org/content/qt6b14h4bv/qt6b14h4bv.pdf |access-date=4 May 2025 }}</ref> [[Charcoal]] is a source of highly stable humus, called [[black carbon]],<ref>{{cite journal |last1=Brodowski |first1=Sonja |last2=Amelung |first2=Wulf |last3=Haumaier |first3=Ludwig |last4=Zech |first4=Wolfgang |title=Black carbon contribution to stable humus in German arable soils |journal=Geoderma |year=2007 |volume=139 |issue=1–2 |pages=220–28 |doi=10.1016/j.geoderma.2007.02.004 |bibcode=2007Geode.139..220B |url=https://www.academia.edu/33858429 |access-date=4 May 2025 }}</ref> which had been used traditionally to improve the fertility of nutrient-poor tropical soils. This very ancient practice, as ascertained in the genesis of [[Amazonian dark earths]], has been renewed and became popular under the name of [[biochar]]. It has been suggested that biochar could be used to sequester more carbon in the fight against the greenhouse effect.<ref>{{cite journal |last1=Criscuoli |first1=Irene |last2=Alberti |first2=Giorgio |last3=Baronti |first3=Silvia |last4=Favilli |first4=Filippo |last5=Martinez |first5=Cristina |last6=Calzolari |first6=Costanza |last7=Pusceddu |first7=Emanuela |last8=Rumpel |first8=Cornelia |last9=Viola |first9=Roberto |last10=Miglietta |first10=Franco |title=Carbon sequestration and fertility after centennial time scale incorporation of charcoal into soil |journal=[[PLOS ONE]] |year=2014 |volume=9 |issue=3 |article-number=e91114 |doi=10.1371/journal.pone.0091114 |pmc=3948733 |pmid=24614647|bibcode=2014PLoSO...991114C |doi-access=free }}</ref>

===Climatological influence===
The production, accumulation and degradation of organic matter are greatly dependent on climate. For example, when a [[Thaw (weather)|thawing]] event occurs, the flux of [[soil gas]]es with atmospheric gases is significantly influenced.<ref>{{cite journal |last1=Kim |first1=Dong Jim |last2=Vargas |first2=Rodrigo |last3=Bond-Lamberty |first3=Ben |last4=Turetsky |first4=Merritt R. |title=Effects of soil rewetting and thawing on soil gas fluxes: a review of current literature and suggestions for future research |journal=[[Biogeosciences]] |year=2012 |volume=9 |issue=7 |pages=2459–83 |doi=10.5194/bg-9-2459-2012 |bibcode=2012BGeo....9.2459K |doi-access=free }}</ref> Temperature, soil moisture and [[topography]] are the major factors affecting the accumulation of organic matter in soils. Organic matter tends to accumulate under wet or cold conditions where [[decomposer]] activity is impeded by low temperature<ref name="Wagai2008">{{cite journal |last1=Wagai |first1=Rota |last2=Mayer |first2=Lawrence M. |last3=Kitayama |first3=Kanehiro |last4=Knicker |first4=Heike |year=2008 |title=Climate and parent material controls on organic matter storage in surface soils: a three-pool, density-separation approach |journal=Geoderma |volume=147 |issue=1–2 |pages=23–33 |doi=10.1016/j.geoderma.2008.07.010 |bibcode=2008Geode.147...23W |url=https://www.academia.edu/20165844 |access-date=4 May 2025 }}</ref> or excess moisture which results in anaerobic conditions.<ref name="Minayeva2008">{{cite journal |last1=Minayeva |first1=Tatiana Y. |last2=Trofimov |first2=Sergey Ya. |last3=Chichagova |first3=Olga A. |last4=Dorofeyeva |first4=E. I. |last5=Sirin |first5=Andrey A. |last6=Glushkov |first6=Igor V. |last7=Mikhailov |first7=N. D. |last8=Kromer |first8=Bernd |year=2008 |title=Carbon accumulation in soils of forest and bog ecosystems of southern Valdai in the Holocene |journal=Biology Bulletin |volume=35 |issue=5 |pages=524–32 |doi=10.1134/S1062359008050142 |bibcode=2008BioBu..35..524M |s2cid=40927739 |url=https://www.researchgate.net/publication/225229436 |access-date=4 May 2025 }}</ref> Conversely, excessive rain and high temperatures of tropical climates enables rapid decomposition of organic matter and leaching of plant nutrients. Forest ecosystems on these soils rely on efficient recycling of nutrients and plant matter by the living plant and microbial biomass to maintain their productivity, a process which is disturbed by human activities.<ref>{{cite journal |last1=Vitousek |first1=Peter M. |last2=Sanford |first2=Robert L. |title=Nutrient cycling in moist tropical forest |journal=[[Annual Review of Ecology and Systematics]] |year=1986 |volume=17 |issue=1 |pages=137–67 |doi=10.1146/annurev.es.17.110186.001033 |bibcode=1986AnRES..17..137V |s2cid=55212899 |url=https://www.researchgate.net/publication/234150505 |access-date=4 May 2025 }}</ref> Excessive slope, in particular in the presence of cultivation for the sake of agriculture, may encourage the erosion of the top layer of soil which holds most of the raw organic material that would otherwise eventually become humus.<ref>{{cite journal |last1=Rumpel |first1=Cornelia |last2=Chaplot |first2=Vincent |last3=Planchon |first3=Olivier |last4=Bernadou |first4=J. |last5=Valentin |first5=Christian |last6=Mariotti |first6=André |title=Preferential erosion of black carbon on steep slopes with slash and burn agriculture |journal=Catena |year=2006 |volume=65 |issue=1 |pages=30–40 |url=https://www.academia.edu/14788543 |doi=10.1016/j.catena.2005.09.005 |bibcode=2006Caten..65...30R |access-date=4 May 2025 }}</ref>

=== Plant residue ===
{{Pie chart
|caption = Typical types and percentages of plant residue components
|value1 = 45
|label1 = Cellulose
|value2 = 20
|label2 = Lignin
|value3 = 18
|label3 = Hemicellulose
|value4 = 8
|label4 = Protein
|value5 = 5
|label5 = Sugars and starches
|value6 = 2
|label6 = Fats and waxes
}}

[[Cellulose]] and [[hemicellulose]] undergo fast decomposition by fungi and bacteria, with a half-life of 12–18&nbsp;days in a temperate climate.<ref name=Paul1997>{{cite book|last1=Paul |first1=Eldor A. |last2=Paustian |first2=Keith H. |last3=Elliott |first3=E. T. |last4=Cole |first4=C. Vernon |title=Soil organic matter in temperate agroecosystems: long-term experiments in North America |date=1997 |publisher=[[CRC Press]] |location=Boca Raton, Florida |isbn=978-0-8493-2802-2 |page=80 |url=https://fr.1lib.sk/book/5955591/2c4ede |access-date=4 May 2025 }}</ref> [[Wood-decay fungus|Brown rot fungi]] can decompose the cellulose and hemicellulose, leaving the [[lignin]] and [[Phenols|phenolic compounds]] behind. [[Starch]], which is an [[energy storage]] system for plants, undergoes fast decomposition by bacteria and fungi. Lignin consists of [[polymers]] composed of 500 to 600 units with a highly branched, [[Amorphous solid|amorphous]] structure, linked to cellulose, hemicellulose and [[pectin]] in [[plant cell walls]]. Lignin undergoes very slow decomposition, mainly by [[white rot]] fungi and [[actinomycetes]]; its half-life under temperate conditions is about six months.<ref name=Paul1997/>

==Horizons==
{{Main|Soil horizon}}

A horizontal layer of the soil, whose physical features, composition and age are distinct from those above and beneath, is referred to as a [[soil horizon]]. The naming of a horizon is based on the type of material of which it is composed. Those materials reflect the duration of specific processes of soil formation. They are labelled using a shorthand notation of letters and numbers which describe the horizon in terms of its colour, size, texture, structure, consistency, root quantity, pH, voids, boundary characteristics and presence of [[Nodule (geology)|nodules]] or [[concretion]]s.<ref>{{cite web |url=https://soilsofcanada.ca/soil-formation/horizons.php |title=Horizons |website=Soils of Canada |access-date=11 May 2025 |archive-url=https://web.archive.org/web/20190922153041/https://soilsofcanada.ca/soil-formation/horizons.php |archive-date=22 September 2019 |url-status=live }}</ref> No soil profile has all the major horizons. Some, called [[entisols]], may have only one horizon or are currently considered as having no horizon, in particular incipient soils from unreclaimed [[mining waste]] deposits,<ref>{{cite journal |last1=Frouz |first1=Jan |last2=Prach |first2=Karel |last3=Pizl |first3=Václav |last4=Háněl |first4=Ladislav |last5=Starý |first5=Josef |last6=Tajovský |first6=Karel |last7=Materna |first7=Jan |last8=Balík |first8=Vladimír |last9=Kalčík |first9=Jiří |last10=Řehounková |first10=Klára |year=2008 |title=Interactions between soil development, vegetation and soil fauna during spontaneous succession in post mining sites |journal=European Journal of Soil Biology |volume=44 |issue=1 |pages=109–21 |url=https://www.academia.edu/14019971 |doi=10.1016/j.ejsobi.2007.09.002 |bibcode=2008EJSB...44..109F |access-date=11 May 2025 }}</ref> [[moraines]],<ref>{{cite journal |last1=Kabala |first1=Cezary |last2=Zapart |first2=Justyna |year=2012 |title=Initial soil development and carbon accumulation on moraines of the rapidly retreating Werenskiold Glacier, SW Spitsbergen, Svalbard archipelago |journal=Geoderma |volume=175–176 |pages=9–20 |url=https://www.academia.edu/31221217 |doi=10.1016/j.geoderma.2012.01.025 |bibcode=2012Geode.175....9K |access-date=11 May 2025 }}</ref> [[volcanic cones]]<ref>{{cite journal |last1=Ahmad |first1=Asmita |last2=Solle |first2=Muchtar Salam |last3=Lopulisa |first3=Christianto  |year=2019 |title=Soil development from volcanic ash based on different pyroclastic composition |journal=Journal of Tropical Soils |volume=24 |issue=3 |pages=135–40 |doi=10.5400/jts.2019.v24i3.135-140 |doi-access=free }}</ref> [[sand dunes]] or [[alluvial terrace]]s.<ref>{{cite journal |last=Huggett |first=Richard J. |year=1998 |title=Soil chronosequences, soil development, and soil evolution: a critical review |journal=Catena |volume=32 |issue=3 |pages=155–72 |url=https://www.academia.edu/2116704 |doi=10.1016/S0341-8162(98)00053-8 |bibcode=1998Caten..32..155H |access-date=11 May 2025 }}</ref> Upper soil horizons may be lacking in truncated soils following wind or water ablation, with concomitant downslope burying of soil horizons, a natural process aggravated by agricultural practices such as tillage.<ref>{{cite journal |last1=De Alba |first1=Saturnio |last2=Lindstrom |first2=Michael |last3=Schumacher |first3=Thomas E. |last4=Malo |first4=Douglas D. |year=2004 |title=Soil landscape evolution due to soil redistribution by tillage: a new conceptual model of soil catena evolution in agricultural landscapes |journal=Catena |volume=58 |issue=1 |pages=77–100 |url=https://www.academia.edu/22300477 |doi=10.1016/j.catena.2003.12.004 |bibcode=2004Caten..58...77D |access-date=11 May 2025 }}</ref> The growth of trees is another source of disturbance, creating a micro-scale heterogeneity which is still visible in soil horizons once trees have died.<ref>{{cite journal |last1=Phillips |first1=Jonathan D. |last2=Marion |first2=Daniel A. |year=2004 |title=Pedological memory in forest soil development |journal=[[Forest Ecology and Management]] |volume=188 |issue=1 |pages=363–80 |url=https://www.srs.fs.usda.gov/pubs/ja/ja_phillips004.pdf |doi=10.1016/j.foreco.2003.08.007 |bibcode=2004ForEM.188..363P |access-date=11 May 2025 }}</ref> By passing from a horizon to another, from the top to the bottom of the soil profile, one goes back in time, with past events registered in soil horizons like in [[sediment]] layers. Sampling [[pollen]], [[testate amoebae]] and plant remains in soil horizons may help to reveal environmental changes (e.g. climate change, [[land use]] change) which occurred in the course of soil formation.<ref>{{cite journal |last1=Mitchell |first1=Edward A.D. |last2=Van der Knaap |first2=Willem O. |last3=Van Leeuwen |first3=Jacqueline F.N. |last4=Buttler |first4=Alexandre |last5=Warner |first5=Barry G. |last6=Gobat |first6=Jean-Michel |year=2001 |title=The palaeoecological history of the Praz-Rodet bog (Swiss Jura) based on pollen, plant macrofossils and testate amoebae(Protozoa) |journal=[[The Holocene]] |volume=11 |issue=1 |pages=65–80 |url=https://www.academia.edu/31915005 |doi=10.1191/095968301671777798 |bibcode=2001Holoc..11...65M |s2cid=131032169 |access-date=11 May 2025 }}</ref> Soil horizons can be dated by several methods such as [[radiocarbon]], using pieces of charcoal provided they are of enough size to escape [[pedoturbation]] by [[earthworm]] activity and other mechanical disturbances.<ref>{{cite journal |last=Carcaillet |first=Christopher |year=2001 |title=Soil particles reworking evidences by AMS <sup>14</sup>C dating of charcoal |journal=[[Comptes Rendus de l'Académie des Sciences, Série IIA]] |volume=332 |issue=1 |pages=21–28 |url=https://fr.1lib.sk/book/50412117/352654 |doi=10.1016/S1251-8050(00)01485-3 |bibcode=2001CRASE.332...21C |access-date=11 May 2025 }}</ref> Fossil soil horizons from [[paleosols]] can be found within [[sedimentary rock]] sequences, allowing the study of past environments.<ref>{{cite journal |last=Retallack |first=Gregory J. |year=1991 |title=Untangling the effects of burial alteration and ancient soil formation |journal=[[Annual Review of Earth and Planetary Sciences]] |volume=19 |issue=1 |pages=183–206 |doi=10.1146/annurev.ea.19.050191.001151 |bibcode=1991AREPS..19..183R |url=https://www.researchgate.net/publication/234148901 |access-date=11 May 2025 }}</ref>

The exposure of parent material to favourable conditions produces mineral soils that are marginally suitable for plant growth, as is the case in eroded soils.<ref>{{cite journal |last1=Bakker |first1=Martha M. |last2=Govers |first2=Gerard |last3=Jones |first3=Robert A. |last4=Rounsevell |first4=Mark D.A. |year=2007 |title=The effect of soil erosion on Europe's crop yields |journal=Ecosystems |volume=10 |issue=7 |pages=1209–19 |doi=10.1007/s10021-007-9090-3 |bibcode=2007Ecosy..10.1209B |doi-access=free }}</ref> The growth of vegetation results in the production of organic residues which fall on the ground as litter for plant aerial parts ([[leaf litter]]) or are directly produced belowground for subterranean plant organs (root litter), and then release [[dissolved organic matter]].<ref>{{cite journal |last1=Uselman |first1=Shauna M. |last2=Qualls |first2=Robert G. |last3=Lilienfein |first3=Juliane |year=2007 |title=Contribution of root vs. leaf litter to dissolved organic carbon leaching through soil |journal=[[Soil Science Society of America Journal]] |volume=71 |issue=5 |pages=1555–63 |url=https://www.academia.edu/34475958 |doi=10.2136/sssaj2006.0386 |bibcode=2007SSASJ..71.1555U |access-date=11 May 2025 }}</ref> The remaining surficial organic layer, called the [[forest floor|O horizon]], produces a more active soil due to the effect of the organisms that live within it. Organisms colonise and break down organic materials, making available nutrients upon which other plants and animals can live.<ref>{{cite journal |last1=Schulz |first1=Stefanie |last2=Brankatschk |first2=Robert |last3=Dümig |first3=Alexander |last4=Kögel-Knabner |first4=Ingrid|author4-link=Ingrid Kögel-Knabner |last5=Schloter |first5=Michae |last6=Zeyer |first6=Josef |year=2013 |title=The role of microorganisms at different stages of ecosystem development for soil formation |journal=[[Biogeosciences]] |volume=10 |issue=6 |pages=3983–96 |doi=10.5194/bg-10-3983-2013 |bibcode=2013BGeo...10.3983S |doi-access=free |hdl=20.500.11850/70776 |hdl-access=free }}</ref> After sufficient time, [[humus]] moves downward and is deposited in a distinctive organic-mineral surface layer called the [[A horizon]], in which organic matter is mixed with mineral matter through the activity of burrowing animals, a process called [[Perturbation (geology)|pedoturbation]]. This natural process does not go to completion in the presence of conditions detrimental to soil life such as strong acidity, cold climate or pollution, stemming in the accumulation of undecomposed organic matter within a single organic horizon overlying the mineral soil<ref>{{cite journal |last1=Gillet |first1=Servane |last2=Ponge |first2=Jean-François |year=2002 |title=Humus forms and metal pollution in soil |journal=European Journal of Soil Science |volume=53 |issue=4 |pages=529–39 |url=https://www.academia.edu/45705588 |doi=10.1046/j.1365-2389.2002.00479.x |bibcode=2002EuJSS..53..529G |s2cid=94900982 |access-date=11 May 2025 }}</ref> and in the juxtaposition of humified organic matter and mineral particles, without intimate mixing, in the underlying mineral horizons.<ref>{{cite journal |last1=Bardy |first1=Marion |last2=Fritsch |first2=Emmanuel |last3=Derenne |first3=Sylvie |last4=Allard |first4=Thierry |last5=do Nascimento |first5=Nadia Régina |last6=Bueno |first6=Guilherme |year=2008 |title=Micromorphology and spectroscopic characteristics of organic matter in waterlogged podzols of the upper Amazon basin |journal=Geoderma |volume=145 |issue=3 |pages=222–30 |doi=10.1016/j.geoderma.2008.03.008 |bibcode=2008Geode.145..222B |url=https://citeseerx.ist.psu.edu/document?repid=rep1&type=pdf&doi=9370526affebf1bc012ec66afdca723fcdd4a940#page=2.43 |access-date=11 May 2025 }}</ref>

==Classification==
{{main|Soil classification}}

One of the first soil classification systems was developed by Russian scientist [[Vasily Dokuchaev]] around 1880.<ref>{{cite web |url=https://fr.scribd.com/doc/206859253/Russian-Chernozem |title=Russian Chernozem |last=Dokuchaev |first=Vasily Vasilyevich |publisher=Israel Program for Scientific Translations |location=Jerusalem, Israel |year=1967 |access-date=18 May 2025 }}</ref> It was modified a number of times by American and European researchers and was developed into the system commonly used until the 1960s. It was based on the idea that soils have a particular morphology based on the materials and factors that form them. In the 1960s, a different classification system began to emerge which focused on [[soil morphology]] instead of parental materials and soil-forming factors. Since then, it has undergone further modifications. The [[World Reference Base for Soil Resources]]<ref name=WRB>{{Cite web |url=https://wrb.isric.org/files/WRB_fourth_edition_2022-12-18_errata_correction_2024-09-24.pdf |title=World Reference Base for Soil Resources, 4th edition |author=IUSS Working Group WRB |year=2022 |publisher=[[International Union of Soil Sciences]] (IUSS), Vienna, Austria |access-date=18 May 2025 }}</ref> aims to establish an international reference base for soil classification.

In the United States, the system of [[USDA soil taxonomy|Soil Taxonomy]]<ref>{{Cite web |title=USDA NRCS Soil Taxonomy |url=https://www.nrcs.usda.gov/resources/guides-and-instructions/soil-taxonomy }}</ref> is used. This system was established by the United States Department of Agriculture: Natural Resource Conversation Service and is currently on its second edition, released in 1999 by the Soil Survey Staff.<ref>''Soil Survey Staff. 1999. Soil taxonomy: A basic system of soil classification for making and interpreting soil surveys. 2nd edition. Natural Resources Conservation Service. U.S. Department of Agriculture Handbook 436.''</ref>

==Uses==
Soil is used in agriculture, where it serves as the anchor and primary nutrient base for plants. The types of soil and available moisture determine the species of plants that can be cultivated. [[Agricultural soil science]] was the primeval domain of soil knowledge, long time before the advent of [[pedology]] in the 19th century. However, as demonstrated by [[aeroponics]], [[aquaponics]] and [[hydroponics]], soil material is not an absolute essential for agriculture, and soilless cropping systems have been claimed as the future of agriculture for an endless growing mankind.<ref>{{cite journal |last1=Sambo |first1=Paolo |last2=Nicoletto |first2=Carlo |last3=Giro |first3=Andrea |last4=Pii |first4=Youry |last5=Valentinuzzi |first5=Fabio |last6=Mimmo |first6=Tanja |last7=Lugli |first7=Paolo |last8=Orzes |first8=Guido |last9=Mazzetto |first9=Fabrizio |last10=Astolfi |first10=Stefania |last11=Terzano |first11=Roberto |last12=Cesco |first12=Stefano |year=2019 |title=Hydroponic solutions for soilless production systems: issues and opportunities in a smart agriculture perspective |journal=[[Frontiers in Plant Science]] |volume=10 |issue=123 |page=923 |doi=10.3389/fpls.2019.00923 |pmid=31396245 |pmc=6668597 |bibcode=2019FrPS...10..923S |doi-access=free }}</ref>

Soil material is also a critical component in [[mining]], [[construction]] and landscape development (also called [[landscape architecture]]) industries.<ref>{{cite book |title=Soils for landscape development: selection, specification and validation |last1=Leake |first1=Simon |last2=Haege |first2=Elke |publisher=[[CSIRO Publishing]] |location=Clayton, Victoria, Australia |year=2014 |isbn=978-0-643-10965-0 |url=https://fr.1lib.sk/book/5450819/567a5e |access-date=18 May 2025 }}</ref> Soil serves as a foundation for most construction projects. The movement of massive volumes of soil can be involved in [[surface mining]], [[road building]] and [[dam]] construction. [[Earth sheltering]] is the architectural practice of using soil for external [[thermal mass]] against building walls. Many [[building material]]s are soil based. Loss of soil through urbanization is growing at a high rate in many areas and can be critical for the maintenance of [[subsistence agriculture]].<ref>{{cite journal |last1=Pan |first1=Xian-Zhang |last2=Zhao |first2=Qi-Guo |year=2007 |title=Measurement of urbanization process and the paddy soil loss in Yixing city, China between 1949 and 2000 |journal=Catena |volume=69 |issue=1 |pages=65–73 |doi=10.1016/j.catena.2006.04.016 |bibcode=2007Caten..69...65P |url=https://www.cern.ac.cn/ftp/0301%20Measurement%20of%20urbanization%20process%20and%20the%20paddy%20soil%20loss%20in%20Yixing%20city,%20China%20between%201949%20and%202000).pdf |access-date=18 May 2025 }}</ref>

Soil resources are critical to the environment, as well as to food and fibre production, producing 98.8% of food consumed by humans.<ref>{{cite journal |last1=Kopittke |first1=Peter M. |last2=Menzies |first2=Neal W. |last3=Wang |first3=Peng |last4=McKenna |first4=Brigid A. |last5=Lombi |first5=Enzo |year=2019 |title=Soil and the intensification of agriculture for global food security |journal=[[Environment International]] |volume=132 |article-number=105078 |doi=10.1016/j.envint.2019.105078 |pmid=31400601 |issn=0160-4120 |url=https://www.researchgate.net/publication/335922138 |bibcode=2019EnInt.13205078K |access-date=18 May 2025 |doi-access=free |hdl=11541.2/138471 |hdl-access=free }}</ref> Soil provides minerals and water to plants according to several processes involved in [[plant nutrition]]. Soil absorbs rainwater and releases it later, thus preventing floods and drought, flood regulation being one of the major [[ecosystem service]]s provided by soil.<ref>{{cite journal |last1=Stürck |first1=Julia |last2=Poortinga |first2=Ate |last3=Verburg |first3=Peter H. |year=2014 |title=Mapping ecosystem services: the supply and demand of flood regulation services in Europe |journal=Ecological Indicators |volume=38 |pages=198–211 |url=https://www.academia.edu/21713698 |doi=10.1016/j.ecolind.2013.11.010 |bibcode=2014EcInd..38..198S |access-date=18 May 2025 |archive-date=14 August 2021 |archive-url=https://web.archive.org/web/20210814121818/http://docs.gip-ecofor.org/public/Sturck_et_al_2014.pdf |url-status=live }}</ref> Soil cleans water as it percolates through it.<ref>{{cite journal |last1=Van Cuyk |first1=Sheila |last2=Siegrist |first2=Robert |last3=Logan |first3=Andrew |last4=Masson |first4=Sarah |last5=Fischer |first5=Elizabeth |last6=Figueroa |first6=Linda |year=2001 |title=Hydraulic and purification behaviors and their interactions during wastewater treatment in soil infiltration systems |journal=[[Water Research]] |volume=35 |issue=4 |pages=953–64 |url=https://www.academia.edu/17525373 |doi=10.1016/S0043-1354(00)00349-3 |pmid=11235891 |bibcode=2001WatRe..35..953V |access-date=18 May 2025 }}</ref> Soil is the habitat for many organisms: the major part of known and unknown [[biodiversity]] is in the soil, in the form of [[earthworm]]s, [[woodlice]], [[millipede]]s, [[centipede]]s, [[snail]]s, [[slug]]s, [[mite]]s, [[springtail]]s, [[Enchytraeidae|enchytraeids]], [[nematode]]s, [[protist]]s), [[bacteria]], [[archaea]], [[Fungus|fungi]] and [[algae]]; and most organisms living above ground have part of them ([[plants]]) or spend part of their [[Biological life cycle|life cycle]] (e.g. [[insects]]) below-ground.<ref>{{cite book |title=European atlas of soil biodiversity |last1=Jeffery |first1=Simon |last2=Gardi |first2=Ciro |last3=Arwyn |first3=Jones |publisher=[[Publications Office of the European Union]] |location=Luxembourg, Luxembourg |year=2010 |isbn=978-92-79-15806-3 |doi=10.2788/94222 |url=https://op.europa.eu/en/publication-detail/-/publication/7161b2a1-f862-4c90-9100-557a62ecb908 |access-date=18 May 2025 }}</ref> Above-ground and below-ground biodiversities are tightly interconnected,<ref name="Ponge2003" /><ref name="De Deyn2005">{{cite journal |last1=De Deyn |first1=Gerlinde B. |last2=Van der Putten |first2=Wim H. |year=2005 |title=Linking aboveground and belowground diversity |journal=[[Trends in Ecology and Evolution]] |volume=20 |issue=11 |pages=625–33 |url=https://www.researchgate.net/publication/7080980 |doi=10.1016/j.tree.2005.08.009 |pmid=16701446 |access-date=18 May 2025 }}</ref> making [[soil protection]] of paramount importance for any [[Environmental restoration|restoration]] or [[Nature conservation|conservation]] plan.

The biological component of soil is an extremely important carbon sink since about 57% of the biotic content is carbon. Even in deserts, [[cyanobacteria]], [[lichen]]s and [[moss]]es form [[biological soil crust]]s which capture and sequester a significant amount of carbon by [[photosynthesis]]. Poor farming and grazing methods have degraded soils and released much of this sequestered carbon to the atmosphere. Restoring the world's soils could offset the effect of increases in [[greenhouse gas emissions]] and slow global warming, while improving crop yields and reducing water needs.<ref>{{cite journal |last1= Hansen |first1=James |last2=Sato |first2=Makiko |last3=Kharecha |first3=Pushker |last4=Beerling |first4=David |last5=Berner |first5=Robert |last6=Masson-Delmotte |first6=Valerie |last7=Pagani |first7=Mark |last8=Raymo |first8=Maureen |last9=Royer |first9=Dana L. |last10=Zachos |first10=James C. |journal=[[Open Atmospheric Science Journal]] |year=2008 |volume=2 |pages=217–31 |title=Target atmospheric CO<sub>2</sub>: where should humanity aim? |issue=1 |arxiv=0804.1126 |bibcode=2008OASJ....2..217H |doi=10.2174/1874282300802010217 |s2cid=14890013 |url=https://benthamopen.com/contents/pdf/TOASCJ/TOASCJ-2-217.pdf |access-date=25 May 2025 }}</ref><ref>{{cite journal |last=Lal |first=Rattan |date=11 June 2004 |title=Soil carbon sequestration impacts on global climate change and food security |journal=[[Science (journal)|Science]] |volume=304 |issue=5677 |pages=1623–27 |doi=10.1126/science.1097396 |pmid=15192216 |bibcode=2004Sci...304.1623L |s2cid=8574723 |url=https://www.academia.edu/59816044 |access-date=25 May 2025 |archive-date=14 August 2021 |archive-url=https://web.archive.org/web/20210814145106/http://www.tinread.usarb.md:8888/jspui/bitstream/123456789/1067/1/soil_carbon.pdf |url-status=live }}</ref><ref>{{cite web |last=Blakeslee |first=Thomas |title=Greening deserts for carbon credits |date=24 February 2010 |access-date=25 May 2025 |publisher=[[Renewable Energy World]] |location=Orlando, Florida, USA |url=https://www.renewableenergyworld.com/om/greening-deserts-for-carbon-credits/#gref |url-status=live |archive-url=https://web.archive.org/web/20121101011735/http://www.renewableenergyworld.com/rea/news/article/2010/02/greening-deserts-for-carbon-credits |archive-date=1 November 2012 }}</ref>

[[Waste management]] often has a soil component. [[Septic drain field]]s treat [[septic tank]] effluent using [[Aerobic organism|aerobic]] soil processes. Land application of [[waste water]] relies on [[soil biology]] to aerobically treat [[Biochemical oxygen demand|BOD]]. Alternatively, [[landfill]]s use soil for [[daily cover]], isolating waste deposits from the atmosphere and preventing unpleasant smells. [[Composting]] is now widely used to treat aerobically solid domestic waste and dried effluents of [[settling basin]]s. Although compost is not soil, biological processes taking place during composting are similar to those occurring during decomposition and humification of soil organic matter.<ref>{{cite journal |last1=Mondini |first1=Claudio |last2=Contin |first2=Marco |last3=Leita |first3=Liviana |last4=De Nobili |first4=Maria |year=2002 |title=Response of microbial biomass to air-drying and rewetting in soils and compost |journal=Geoderma |volume=105 |issue=1–2 |pages=111–24 |url=https://www.academia.edu/5321925 |doi=10.1016/S0016-7061(01)00095-7 |bibcode=2002Geode.105..111M |access-date=25 May 2025 }}</ref>

Organic soils, especially [[peat]], serve as a significant fuel and [[horticulture|horticultural]] resource. Peat soils are also commonly used for the sake of agriculture in Nordic countries, because peatland sites, when drained, provide fertile soils for food production.<ref>{{cite web |title=Peatlands and farming |date=6 July 2020 |access-date=25 May 2025 |publisher=[[National Farmers' Union of England and Wales]] |location=Stoneleigh, United Kingdom |url=https://www.countrysideonline.co.uk/food-and-farming/protecting-the-environment/peatlands-and-farming |archive-url=https://web.archive.org/web/20200514100050/https://www.countrysideonline.co.uk/food-and-farming/protecting-the-environment/peatlands-and-farming/ |archive-date=14 May 2020 }}</ref> However, wide areas of peat production, such as rain-fed [[sphagnum]] [[bog]]s, also called [[blanket bog]]s or [[raised bog]]s, are now protected because of their patrimonial interest. As an example, [[Flow Country]], covering 4,000 square kilometres of rolling expanse of blanket bogs in Scotland, is now recognized as a [[UNESCO]] [[World Heritage Site]]. Under present-day global warming peat soils are thought to be involved in a self-reinforcing (positive feedback) process of increased emission of greenhouse gases ([[methane]] and [[carbon dioxide]]) and increased temperature,<ref>{{cite journal |last1=Van Winden |first1=Julia F. |last2=Reichart |first2=Gert-Jan |last3=McNamara |first3=Niall P. |last4=Benthien |first4=Albert |last5=Sinninghe Damste |first5=Jaap S. |journal=[[PLoS ONE]] |year=2012 |volume=7 |issue=6 |article-number=e39614 |title=Temperature-induced increase in methane release from peat bogs: a mesocosm experiment |doi=10.1371/journal.pone.0039614 |pmid=22768100 |pmc=3387254 |bibcode=2012PLoSO...739614V |doi-access=free }}</ref> a contention which is still under debate when replaced at field scale and including stimulated plant growth.<ref>{{cite journal |last1=Davidson |first1=Eric A. |last2=Janssens |first2=Ivan A. |year=2006 |title=Temperature sensitivity of soil carbon decomposition and feedbacks to climate change |journal=[[Nature (journal)|Nature]] |volume=440 |issue=7081 |pages=165–73 |doi=10.1038/nature04514 |pmid=16525463 |bibcode=2006Natur.440..165D |s2cid=4404915 |url=https://www.researchgate.net/publication/7253750 |access-date=25 May 2025 }}</ref>

[[Geophagy]] is the practice of eating soil-like substances. Both animals and humans occasionally consume soil for medicinal, recreational, or religious purposes.<ref>{{cite journal |last=Abrahams |first=Pter W. |year=1997 |title=Geophagy (soil consumption) and iron supplementation in Uganda |journal=[[Tropical Medicine and International Health]] |volume=2 |issue=7 |pages=617–23 |doi=10.1046/j.1365-3156.1997.d01-348.x |pmid=9270729 |s2cid=19647911 |doi-access=free }}</ref> It has been shown that some [[monkeys]] consume soil, together with their preferred food (tree [[foliage]] and [[fruits]]), in order to alleviate tannin toxicity.<ref name="Setz1999">{{cite journal|last1=Setz |first1=Eleonore Zulnara Freire |last2=Enzweiler |first2=Jacinta |last3=Solferini |first3=Vera Nisaka |last4=Amêndola |first4=Monica Pimenta |last5=Berton |first5=Ronaldo Severiano |year=1999 |title=Geophagy in the golden-faced saki monkey (Pithecia pithecia chrysocephala) in the Central Amazon |journal=[[Journal of Zoology]] |volume=247 |issue=1 |pages=91–103 |doi=10.1111/j.1469-7998.1999.tb00196.x |url=https://www.academia.edu/26464333 |access-date=25 May 2025 }}</ref>

Soils filter and purify water and affect its chemistry. Rain water and pooled water from [[pond]]s, [[lake]]s and [[river]]s percolate through the soil horizons and the upper [[Stratum|rock strata]], thus becoming [[groundwater]]. [[Pest (organism)|Pests]] ([[virus]]es) and [[pollutant]]s, such as [[persistent organic pollutant]]s ([[chlorinated]] [[pesticide]]s, [[polychlorinated biphenyl]]s), oils ([[hydrocarbon]]s), heavy metals ([[lead]], zinc, [[cadmium]]), and excess nutrients (nitrates, [[sulfate]]s, phosphates) are filtered out by the soil.<ref name="Kohne2009">{{cite journal |last1=Kohne |first1=John Maximilian |last2=Koehne |first2=Sigrid |last3=Simunek |first3=Jirka |date=2009 |title=A review of model applications for structured soils: a) Water flow and tracer transport |journal=Journal of Contaminant Hydrology |volume=104 |pages=4–35 |doi=10.1016/j.jconhyd.2008.10.002 |pmid=19012994 |issue=1–4 |bibcode=2009JCHyd.104....4K |url=https://www.pc-progress.com/documents/jirka/ko-ko_sim_2008_jcontamhydrol.pdf |url-status=live |archive-url=https://web.archive.org/web/20171107005433/http://www.soil.tu-bs.de/lehre/Master.Monitoring/2009/Daten/5_Literatur/A%20review%20of-Koehne-2009.pdf |archive-date=7 November 2017 |citeseerx=10.1.1.468.9149 |access-date=25 May 2025 }}</ref> Soil organisms [[metabolise]] them or immobilise them in their biomass and necromass,<ref name="Diplock2009">{{cite journal |last1=Diplock |first1=Elizabeth E. |last2=Mardlin |first2=Dave P. |last3=Killham |first3=Kenneth S. |last4=Paton |first4=Graeme Iain |year=2009 |title=Predicting bioremediation of hydrocarbons: laboratory to field scale |journal=[[Environmental Pollution (journal)|Environmental Pollution]] |volume=157 |pages=1831–40 |doi=10.1016/j.envpol.2009.01.022 |pmid=19232804 |issue=6 |bibcode=2009EPoll.157.1831D |url=https://fr.1lib.sk/book/45701836/eb7e2a |access-date=25 May 2025 }}</ref> thereby incorporating them into stable humus.<ref name="Moeckel2008">{{cite journal |last1=Moeckel |first1=Claudia |last2=Nizzetto |first2=Luca |last3=Di Guardo |first3=Antonio |last4=Steinnes |first4=Eiliv |last5=Freppaz |first5=Michele |last6=Filippa |first6=Gianluca |last7=Camporini |first7=Paolo |last8=Benner |first8=Jessica |last9=Jones |first9=Kevin C. |date=2008 |title=Persistent organic pollutants in boreal and montane soil profiles: distribution, evidence of processes and implications for global cycling |journal=[[Environmental Science and Technology]] |volume=42 |pages=8374–80 |doi=10.1021/es801703k |pmid=19068820 |issue=22 |bibcode=2008EnST...42.8374M |hdl=11383/8693 |url=https://www.academia.edu/15598352 |access-date=25 May 2025 |hdl-access=free }}</ref> The physical integrity of soil is also a prerequisite for avoiding [[landslide]]s in rugged landscapes.<ref name="Rezaei2009">{{cite journal |last1=Rezaei |first1=Khalil |last2=Guest |first2=Bernard |last3=Friedrich |first3=Anke |last4=Fayazi |first4=Farajollah |last5=Nakhaei |first5=Mohamad |last6=Aghda |first6=Seyed Mahmoud Fatemi |last7=Beitollahi |first7=Ali |date=2009 |title=Soil and sediment quality and composition as factors in the distribution of damage at the December 26, 2003, Bam area earthquake in SE Iran (M (s)=6.6) |journal=Journal of Soils and Sediments |volume=9 |issue=1 |pages=23–32 |doi=10.1007/s11368-008-0046-9 |bibcode=2009JSoSe...9...23R |s2cid=129416733 |url=https://www.researchgate.net/publication/225752596 |access-date=25 May 2025 }}</ref>

==Degradation==
{{Main|Soil retrogression and degradation|Soil conservation}}
[[Land degradation]] is a human-induced or natural process which impairs the capacity of [[land (economics)|land]] to function.<ref>{{cite journal |last1=Johnson |first1=Dan L. |last2=Ambrose |first2=Stanley H. |last3=Bassett |first3=Thomas J. |last4=Bowen |first4=Merle L. |last5=Crummey |first5=Donald E. |last6=Isaacson |first6=John S. |last7=Johnson |first7=David N. |last8=Lamb |first8=Peter |last9=Saul |first9=Mahir |last10=Winter-Nelson |first10=Alex E. |year=1997 |title=Meanings of environmental terms |url=https://www.researchgate.net/publication/240784159 |journal=[[Journal of Environmental Quality]] |volume=26 |issue=3 |pages=581–89 |doi=10.2134/jeq1997.00472425002600030002x |bibcode=1997JEnvQ..26..581J |access-date=26 May 2025 }}</ref> [[Soil degradation]] involves [[Soil acidification|acidification]], [[soil contamination|contamination]], [[desertification]], [[erosion]] or [[Soil salinity|salination]].<ref>{{cite book |last=Oldeman |first=L. Roel |year=1993 |chapter=Global extent of soil degradation |title=ISRIC Bi-Annual Report 1991–1992 |pages=19–36 |chapter-url=https://edepot.wur.nl/299739 |publisher=[[International Soil Reference and Information Centre]](ISRIC) |location=Wageningen, The Netherlands |access-date=26 May 2025 }}</ref>

=== Acidification ===
Soil acidification is beneficial in the case of [[alkaline soil]]s, but it degrades land when it lowers [[crop productivity]], soil biological activity and increases soil vulnerability to [[contamination]] and [[erosion]]. Soils are initially acid and remain such when their parent materials are low in basic [[cation]]s (calcium, magnesium, potassium and [[sodium]]). On parent materials richer in [[mineral weathering|weatherable minerals]] acidification occurs when basic cations are [[Leaching (pedology)|leached]] from the soil profile by rainfall or exported by the harvesting of forest or agricultural crops. Soil acidification is accelerated by the use of acid-forming [[nitrogenous fertilizer]]s and by the effects of [[acid precipitation]]. [[Deforestation]] is another cause of soil acidification, mediated by increased leaching of soil nutrients in the absence of [[tree canopies]].<ref>{{cite book |last1=Sumner |first1=Malcolm E. |last2=Noble |first2=Andrew D. |year=2003 |chapter=Soil acidification: the world story |title=Handbook of soil acidity |pages=1–28 |editor-last=Rengel |editor-first=Zdenko |chapter-url=https://fr.1lib.sk/book/94578788/32bb8a |publisher=[[Marcel Dekker]] |location=New York, New York, USA |isbn=978-0-429-22309-9 |access-date=29 August 2021 |archive-date=14 August 2021 |archive-url=https://web.archive.org/web/20210814115102/https://pdf-drive.com/pdf/Zdenko20Rengel20-20Handbook20of20Soil20Acidity2028Books20in20Soils2C20Plants2C20and20the20Environment292028200329.pdf#page=16 |url-status=live }}</ref>

===Contamination===
Soil [[contamination]] at low levels is often within a soil's capacity to treat and assimilate [[waste]] material. [[Soil biota]] can treat waste by transforming it, mainly through microbial [[Enzyme|enzymatic]] activity.<ref>{{cite journal |last1=Karam |first1=Jean |last2=Nicell |first2=James A. |year=1997 |title=Potential applications of enzymes in waste treatment |url=https://www.researchgate.net/publication/30002097 |journal=[[Journal of Chemical Technology & Biotechnology]] |volume=69 |issue=2 |pages=141–53 |doi=10.1002/(SICI)1097-4660(199706)69:2<141::AID-JCTB694>3.0.CO;2-U |bibcode=1997JCTB...69..141K |access-date=26 May 2025 }}</ref> Soil organic matter and soil minerals can adsorb the waste material and decrease its [[toxicity]],<ref>{{cite journal |last1=Sheng |first1=Guangyao |last2=Johnston |first2=Cliff T. |last3=Teppen |first3=Brian J. |last4=Boyd |first4=Stephen A. |year=2001 |title=Potential contributions of smectite clays and organic matter to pesticide retention in soils |url=https://www.academia.edu/4875079 |journal=[[Journal of Agricultural and Food Chemistry]] |volume=49 |issue=6 |pages=2899–907 |doi=10.1021/jf001485d |pmid=11409985 |bibcode=2001JAFC...49.2899S |access-date=26 May 2025 }}</ref> although when in colloidal form they may transport the adsorbed contaminants to subsurface environments.<ref>{{cite journal |last1=Sprague |first1=Lori A. |last2=Herman |first2=Janet S. |last3=Hornberger |first3=George M. |last4=Mills |first4=Aaron L. |year=2000 |title=Atrazine adsorption and colloid-facilitated transport through the unsaturated zone |url=https://fr.1lib.sk/book/106133437/dae129 |journal=[[Journal of Environmental Quality]] |volume=29 |issue=5 |pages=1632–41 |doi=10.2134/jeq2000.00472425002900050034x |bibcode=2000JEnvQ..29.1632S |access-date=26 May 2025 |archive-date=14 August 2021 |archive-url=https://web.archive.org/web/20210814121821/https://lmecol.evsc.virginia.edu/pubs/73-Sprague_JEQ2000.pdf |url-status=live }}</ref> Many waste treatment processes rely on this natural [[bioremediation]] capacity. Exceeding treatment capacity can damage soil biota and limit soil function. Derelict soils occur where industrial contamination or other development activity damages the soil to such a degree that the land cannot be used safely or productively. [[Environmental remediation|Remediation]] of derelict soil uses principles of geology, physics, chemistry and biology to degrade, attenuate, isolate or remove soil contaminants to restore [[soil functions]] and values. Techniques include [[Leaching (chemistry)|leaching]], [[air sparging]], [[soil conditioner]]s, [[phytoremediation]], [[bioremediation]] and [[In situ bioremediation|Monitored Natural Attenuation]]. An example of diffuse pollution with contaminants is [[copper]] accumulation in [[vineyard]]s and [[orchard]]s to which [[fungicide]]s are repeatedly applied, even in [[organic farming]].<ref>{{cite journal |last1=Ballabio |first1=Cristiano |last2=Panagos |first2=Panos |last3=Lugato |first3=Emanuele |last4=Huang |first4=Jen-How |last5=Orgiazzi |first5=Alberto |last6=Jones |first6=Arwyn |last7=Fernández-Ugalde |first7=Oihane |last8=Borrelli |first8=Pasquale |last9=Montanarella |first9=Luca |date=15 September 2018 |title=Copper distribution in European topsoils: an assessment based on LUCAS soil survey |journal=[[Science of the Total Environment]] |volume=636 |pages=282–98 |doi=10.1016/j.scitotenv.2018.04.268 |pmid=29709848 |issn=0048-9697 |bibcode=2018ScTEn.636..282B |doi-access=free }}</ref>

[[Microfiber|Microfibres]] from synthetic textiles are another type of plastic soil contamination, 100% of agricultural soil samples from southwestern China contained plastic particles, 92% of which were microfibres. Sources of microfibres likely included string or [[twine]], as well as [[irrigation]] water in which clothes had been washed.<ref name="auto">{{cite web |date=21 October 2021 |title=Drowning in plastics: marine litter and plastic waste vital graphics |url=https://www.unep.org/resources/report/drowning-plastics-marine-litter-and-plastic-waste-vital-graphics |access-date=26 May 2025 |website=[[United Nations Environment Programme]] |language=en }}</ref>

The application of [[biosolids]] from [[sewage sludge]] and [[compost]] can introduce [[microplastics]] to soils. This adds to the burden of microplastics from other sources (e.g. the atmosphere). Approximately half the sewage sludge in Europe and North America is applied to agricultural land. In Europe it has been estimated that for every million inhabitants 113 to 770 tonnes of microplastics are added to agricultural soils each year.<ref name="auto"/>

===Desertification===
[[File:Soil erosion, Southfield - geograph.org.uk - 367917.jpg|thumb|Desertification]]

[[Desertification]], an environmental process of ecosystem degradation in arid and semi-arid regions, is often caused by badly adapted human activities such as [[overgrazing]] or excess harvesting of [[firewood]]. It is a common misconception that [[drought]] causes desertification.<ref>{{cite journal |last=Le Houérou |first=Henry N. |year=1996 |title=Climate change, drought and desertification |journal=[[Journal of Arid Environments]] |volume=34 |issue=2 |pages=133–85 |doi=10.1006/jare.1996.0099 |bibcode=1996JArEn..34..133L |url=https://www7.nau.edu/mpcer/direnet/publications/publications_l/files/LeHouerou_1996.pdf |access-date=26 May 2025 }}</ref> While droughts are common in [[Aridity|arid]] and [[Semi-arid climate|semiarid]] lands, well-managed lands can recover from drought when the rains return. [[Soil management]] tools include maintaining soil nutrient and organic matter levels, reduced tillage and increased cover.<ref>{{cite journal |last1=Lyu |first1=Yanli |last2=Shi |first2=Peijun |last3=Han |first3=Guoyi |last4=Liu |first4=Lianyou |last5=Guo |first5=Lanlan |last6=Hu |first6=Xia |last7=Zhang |first7=Guoming |year=2020 |title=Desertification control practices in China |journal=[[Sustainability (journal)|Sustainability]] |volume=12 |issue=8 |page=3258 |doi=10.3390/su12083258 |issn=2071-1050 |doi-access=free |bibcode=2020Sust...12.3258L }}</ref> These practices help to control [[erosion]] and maintain productivity during periods when moisture is available. Continued land abuse during droughts, however, increases [[land degradation]]. Increased population and [[livestock]] pressure on [[marginal land]]s accelerates desertification.<ref>{{cite journal |last1=Kéfi |first1=Sonia |last2=Rietkerk |first2=Max |last3=Alados |first3=Concepción L. |last4=Pueyo |first4=Yolanda |last5=Papanastasis |first5=Vasilios P. |last6=El Aich |first6=Ahmed |last7=De Ruiter |first7=Peter C. |year=2007 |title=Spatial vegetation patterns and imminent desertification in Mediterranean arid ecosystems |journal=[[Nature (journal)|Nature]] |volume=449 |issue=7159 |pages=213–17 |doi=10.1038/nature06111 |pmid=17851524 |bibcode=2007Natur.449..213K |hdl=1874/25682 |s2cid=4411922 |url=https://www.researchgate.net/publication/232801317 |access-date=26 May 2025 |hdl-access=free }}</ref> It is now questioned whether present-day [[Climate change|climate warming]] will favour or disfavour desertification, with contradictory reports about predicted rainfall trends associated with increased temperature, and strong discrepancies among regions, even in the same country.<ref>{{cite journal |last1=Wang |first1=Xunming |last2=Yang |first2=Yi |last3=Dong |first3=Zhibao |last4=Zhang |first4=Caixia |year=2009 |title=Responses of dune activity and desertification in China to global warming in the twenty-first century |journal=[[Global and Planetary Change]] |volume=67 |issue=3–4 |pages=167–85 |doi=10.1016/j.gloplacha.2009.02.004 |bibcode=2009GPC....67..167W |url=https://www.researchgate.net/publication/229103975 |access-date=26 May 2025 }}</ref>

===Erosion===
[[File:Riparian buffer on Bear Creek in Story County, Iowa.JPG|thumb|upright|Erosion control]]

[[Erosion]] of soil is caused by [[Water erosion#Rainfall|water]], [[Water erosion#Wind erosion|wind]], [[Water erosion#Glaciers|ice]], and [[Water erosion#Mass movement|movement in response to gravity]]. More than one kind of erosion can occur simultaneously. Erosion is distinguished from [[weathering]], since erosion also transports eroded soil away from its place of origin (soil in transit may be described as [[sediment]]). Erosion is an intrinsic natural process, but in many places it is greatly increased by human activity, especially unsuitable [[land use]] practices.<ref>{{cite journal |last1=Yang |first1=Dawen |last2=Kanae |first2=Shinjiro |last3=Oki |first3=Taikan |last4=Koike |first4=Toshio |last5=Musiake |first5=Katumi |year=2003 |title=Global potential soil erosion with reference to land use and climate changes |journal=Hydrological Processes |volume=17 |issue=14 |pages=2913–28 |doi=10.1002/hyp.1441 |bibcode=2003HyPr...17.2913Y |s2cid=129355387 |url=https://fr.1lib.sk/book/32752143/3358c1 |access-date=26 May 2025 |archive-date=18 August 2021 |archive-url=https://web.archive.org/web/20210818043117/https://www.oieau.org/eaudoc/system/files/documents/38/191115/191115_doc.pdf |url-status=live }}</ref> These include [[agriculture|agricultural]] activities which leave the soil bare during times of heavy rain or strong winds, [[overgrazing]], [[deforestation]], and improper [[construction]] activity. Improved management can limit erosion. [[Soil conservation#Erosion prevention|Soil conservation techniques]] which are employed include changes of land use (such as replacing erosion-prone [[crop]]s with [[grass]] or other soil-binding plants), changes to the timing or type of agricultural operations, [[Terrace (agriculture)|terrace]] building, use of erosion-suppressing cover materials (including [[Cover crop#Water management|cover crops]] and other plants), limiting disturbance during construction, and avoiding construction during erosion-prone periods and in erosion-prone places such as steep slopes.<ref>{{cite journal |last1=Sheng |first1=Jian-an |last2=Liao |first2=An-zhong |year=1997 |title=Erosion control in South China |journal=Catena |issn=0341-8162 |volume=29 |issue=2 |pages=211–21 |doi=10.1016/S0341-8162(96)00057-4 |bibcode=1997Caten..29..211S |url=https://fr.1lib.sk/book/50141086/129ff4 |access-date=26 May 2025 }}</ref> Historically, one of the best examples of large-scale soil erosion due to unsuitable land-use practices is wind erosion (the so-called [[Dust Bowl|dust bowl]]) which ruined American and Canadian prairies during the 1930s, when immigrant farmers, encouraged by the federal government of both countries, settled and converted the original [[shortgrass prairie]] to [[agricultural crops]] and [[cattle ranching]].

A serious and long-running water erosion problem occurs in [[China]], on the middle reaches of the [[Yellow River]] and the upper reaches of the [[Yangtze River]]. From the Yellow River, over 1.6&nbsp;billion tons of sediment flow each year into the ocean. The sediment originates primarily from water erosion ([[gully]] erosion) in the [[Loess Plateau]] region of northwest China.<ref>{{cite journal |last1=Ran |first1=Lishan |last2=Lu |first2=Xi Xi |last3=Xin |first3=Zhongbao |year=2014 |title=Erosion-induced massive organic carbon burial and carbon emission in the Yellow River basin, China |journal=[[Biogeosciences]] |volume=11 |issue=4 |pages=945–59 |doi=10.5194/bg-11-945-2014 |bibcode=2014BGeo...11..945R |hdl=10722/228184 |hdl-access=free |doi-access=free }}</ref>

Soil piping is a particular form of soil erosion that occurs below the soil surface.<ref>{{cite journal |last1=Verachtert |first1=Els |last2=Van den Eeckhaut |first2=Miet |last3=Poesen |first3=Jean |last4=Deckers |first4=Jozef |year=2010 |title=Factors controlling the spatial distribution of soil piping erosion on loess-derived soils: a case study from central Belgium |journal=[[Geomorphology (journal)|Geomorphology]] |volume=118 |issue=3 |pages=339–48 |doi=10.1016/j.geomorph.2010.02.001 |bibcode=2010Geomo.118..339V |url=https://lirias.kuleuven.be/retrieve/109942 |access-date=26 May 2025 }}</ref> It causes [[levee]] and [[dam]] failure, as well as [[Sinkhole|sink hole]] formation. Turbulent flow removes soil starting at the mouth of the [[Seep (hydrology)|seep]] flow and the [[subsoil]] erosion advances up-gradient.<ref>{{cite journal |last=Jones |first=Anthony |title=Soil piping and stream channel initiation |journal=[[Water Resources Research]] |volume=7 |issue=3 |pages=602–10 |year=1976 |doi=10.1029/WR007i003p00602 |bibcode=1971WRR.....7..602J |url=https://fr.1lib.sk/book/52873995/41e35e |access-date=26 May 2025 }}</ref> The term [[sand boil]] is used to describe the appearance of the discharging end of an active soil pipe.<ref>{{cite web |last=Dooley |first=Alan |title=Sandboils 101: corps has experience dealing with common flood danger |website=Engineer Update |publisher=[[United States Army Corps of Engineers|US Army Corps of Engineers]] |date=June 2006 |url=http://www.hq.usace.army.mil/cepa/pubs/jun06/story8.htm |archive-url=https://web.archive.org/web/20080418185527/http://www.hq.usace.army.mil/cepa/pubs/jun06/story8.htm |archive-date=18 April 2008 }}</ref>

===Salination===
[[Soil salination]] is the accumulation of free [[salt]]s to such an extent that it leads to degradation of the agricultural value of soils and vegetation. Consequences include [[corrosion]] damage, reduced plant growth, erosion due to loss of [[plant cover]] and [[soil structure]], and [[water quality]] problems due to [[sedimentation]]. Salination occurs due to a combination of natural and human-caused processes. Arid conditions favour salt accumulation. This is especially apparent when soil parent material is saline. [[Surface irrigation|Irrigation]] of arid lands is especially problematic.<ref>{{cite web |last=Oosterbaan |first=Roland J. |title=Effectiveness and social/environmental impacts of irrigation projects: a critical review |series=Annual Reports of the International Institute for Land Reclamation and Improvement (ILRI) |year=1988 |pages=18–34 |location=Wageningen, The Netherlands |url=https://www.waterlog.info/pdf/irreff.pdf |url-status=live |archive-url=https://web.archive.org/web/20090219070320/http://waterlog.info/pdf/irreff.pdf |archive-date=19 February 2009 |access-date=26 May 2025 }}</ref> All irrigation water has some level of salinity. Irrigation, especially when it involves leakage from canals and overirrigation in the field, often raises the underlying [[water table]]. Rapid salination occurs when the land surface is within the [[capillary fringe]] of saline [[groundwater]]. [[Soil salinity control]] involves [[watertable control]] and [[leaching model|flushing]] with higher levels of applied water in combination with [[tile drainage]] or another form of [[Drainage system (agriculture)|subsurface drainage]].<ref>{{cite book |title=Drainage manual: a guide to integrating plant, soil, and water relationships for drainage of irrigated lands |year=1993 |publisher=[[United States Department of the Interior]], [[United States Bureau of Reclamation|Bureau of Reclamation]] |location=Washington, D.C. |url=https://www.usbr.gov/tsc/techreferences/mands/mands-pdfs/DrainMan.pdf |isbn=978-0-16-061623-5 |access-date=26 May 2025 }}</ref><ref name="Waterlog">{{cite web |last=Oosterbaan |first=Roland J. |url=http://www.waterlog.info |title=Waterlogging, soil salinity, field irrigation, plant growth, subsurface drainage, groundwater modelling, surface runoff, land reclamation, and other crop production and water management aspects |access-date=26 May 2025 |url-status=live |archive-url=https://web.archive.org/web/20100816225219/http://www.waterlog.info/ |archive-date=16 August 2010 }}</ref>

== Reclamation ==
{{Main|Soil regeneration}}
Soils which contain high levels of particular clays with high swelling properties, such as [[smectite]]s, are often very fertile. For example, the smectite-rich [[Paddy field|paddy]] soils of Thailand's [[Central Thailand|Central Plains]] are among the most productive in the world. However, the overuse of mineral nitrogen [[fertilizer]]s and pesticides in [[Irrigation|irrigated]] intensive [[Rice production in Thailand|rice production]] has endangered these soils, forcing farmers to implement [[integrated farming|integrated practices]] based on Cost Reduction Operating Principles.<ref>{{cite journal |last1=Stuart |first1=Alexander M. |last2=Pame |first2=Anny Ruth P. |last3=Vithoonjit |first3=Duangporn |last4=Viriyangkura |first4=Ladda |last5=Pithuncharurnlap |first5=Julmanee |last6=Meesang |first6=Nisa |last7=Suksiri |first7=Prarthana |last8=Singleton |first8=Grant R. |last9=Lampayan |first9=Rubenito M. |year=2018 |title=The application of best management practices increases the profitability and sustainability of rice farming in the central plains of Thailand |url=https://fr.1lib.sk/book/95909243/ad91a5 |journal=Field Crops Research |volume=220 |pages=78–87 |doi=10.1016/j.fcr.2017.02.005 |bibcode=2018FCrRe.220...78S |access-date=26 May 2025 }}</ref>

Many farmers in tropical areas, however, struggle to retain organic matter and clay in the soils they work. In recent years, for example, productivity has declined and soil erosion has increased in the low-clay soils of northern Thailand, following the abandonment of [[shifting cultivation]] for a more permanent land use.<ref>{{cite journal |last1=Turkelboom |first1=Francis |last2=Poesen |first2=Jean |last3=Ohler |first3=Ilse |last4=Van Keer |first4=Koen |last5=Ongprasert |first5=Somchai |last6=Vlassak |first6=Karel |year=1997 |title=Assessment of tillage erosion rates on steep slopes in northern Thailand |url=https://www.academia.edu/17993140 |journal=Catena |volume=29 |issue=1 |pages=29–44 |doi=10.1016/S0341-8162(96)00063-X |bibcode=1997Caten..29...29T |access-date=26 May 2025 }}</ref> Farmers initially responded by adding organic matter and clay from [[Mound-building termites|termite mound]] material, but this was [[Sustainability|unsustainable]] in the long-term because of rarefaction of termite mounds. Scientists experimented with adding [[bentonite]], one of the [[smectite]] family of clays, to the soil. In field trials, conducted by scientists from the [[International Water Management Institute]] (IWMI) in cooperation with [[Khon Kaen University]] and local farmers, this had the effect of helping retain water and nutrients. Supplementing the farmer's usual practice with a single application of {{convert|200|kg/rai|kg/hectare lb/acre|lk=in}} of bentonite resulted in an average yield increase of 73%.<ref>{{cite journal |last1=Saleth |first1=Rathinasamy Maria |last2=Inocencio |first2=Arlene |last3=Noble |first3=Andrew |last4=Ruaysoongnern |first4=Sawaeng |year=2009 |title=Economic gains of improving soil fertility and water holding capacity with clay application: the impact of soil remediation research in Northeast Thailand |url=https://ageconsearch.umn.edu/record/53064/files/RR130.pdf |journal=Journal of Development Effectiveness |volume=1 |issue=3 |pages=336–52 |doi=10.1080/19439340903105022 |s2cid=18049595 |access-date=26 May 2025 }}</ref> Other studies showed that applying bentonite to degraded sandy soils reduced the risk of crop failure during drought years.<ref>{{cite journal |last1=Semalulu |first1=Onesmus |last2=Magunda |first2=Matthias |last3=Mubiru |first3=Drake N. |year=2015 |title=Amelioration of sandy soils in drought stricken areas through use of Ca-bentonite |journal=Uganda Journal of Agricultural Sciences |volume=16 |issue=2 |pages=195–205 |doi=10.4314/ujas.v16i2.5 |doi-access=free }}</ref>

In 2008, three years after the initial trials, IWMI scientists conducted a survey among 250 farmers in northeast Thailand, half of whom had applied bentonite to their fields. The average improvement for those using the clay addition was 18% higher than for non-clay users. Using the clay had enabled some farmers to switch to growing vegetables, which need more fertile soil. This helped to increase their income. The researchers estimated that 200 farmers in northeast Thailand and 400 in [[Cambodia]] had adopted the use of clays, and that a further 20,000 farmers were introduced to the new technique.<ref name="Water Management Institute2010">{{cite journal |year=2010 |title=Improving soils and boosting yields in Thailand |doi=10.5337/2011.0031 |journal=Success Stories |issue=2 |author=[[International Water Management Institute]] |doi-access=free |hdl=10568/36503 |hdl-access=free }}</ref>

If the soil is too high in clay or salts (e.g. [[saline sodic soil]]), adding [[gypsum]], washed river sand and organic matter (e.g.[[municipal solid waste]]) will balance the composition.<ref>{{cite journal |last1=Prapagar |first1=Komathy |last2=Indraratne |first2=Srimathie P. |last3=Premanandharajah |first3=Punitha |year=2012 |title=Effect of soil amendments on reclamation of saline-sodic soil |journal=Tropical Agricultural Research |volume=23 |issue=2 |pages=168–76 |doi=10.4038/tar.v23i2.4648 |doi-access=free }}</ref>

Adding organic matter, like [[ramial chipped wood]] or [[compost]], to soil which is depleted in nutrients and too high in sand will boost its quality and improve production.<ref>{{cite web |last1=Lemieux |first1=Gilles |last2=Germain |first2=Diane |title=Ramial chipped wood: the clue to a sustainable fertile soil |publisher=[[Université Laval]], Département des Sciences du Bois et de la Forêt, Québec, Canada |date=December 2000 |url=https://www.researchgate.net/publication/228364133 |access-date=26 May 2025 |archive-date=28 September 2021 |archive-url=https://web.archive.org/web/20210928080056/https://www.healthy-vegetable-gardening.com/support-files/rcw-the-clue-to-a-sustainable-fertile-soil.pdf |url-status=live }}</ref><ref>{{cite journal |last1=Arthur |first1=Emmanuel |last2=Cornelis |first2=Wim |last3=Razzaghi |first3=Fatemeh |year=2012 |title=Compost amendment of sandy soil affects soil properties and greenhouse tomato productivity |url=https://www.academia.edu/31660161 |journal=Compost Science and Utilization |volume=20 |issue=4 |pages=215–21 |doi=10.1080/1065657X.2012.10737051 |bibcode=2012CScUt..20..215A |s2cid=96896374 |access-date=26 May 2025 }}</ref>

Special mention must be made of the use of [[charcoal]], and more generally [[biochar]] to improve nutrient-poor tropical soils, a process based on the higher fertility of anthropogenic [[Pre-Columbian era|pre-Columbian]] Amazonian [[Dark earth|Dark Earths]], also called [[Terra Preta]] de Índio, due to interesting physical and chemical properties of soil [[black carbon]] as a source of stable humus.<ref>{{cite journal |last1=Glaser |first1=Bruno |last2=Haumaier |first2=Ludwig |last3=Guggenberger |first3=Georg |last4=Zech |first4=Wolfgang |year=2001 |title=The 'Terra Preta' phenomenon: a model for sustainable agriculture in the humid tropics |url=https://www.researchgate.net/publication/12032464 |journal=[[The Science of Nature|Naturwissenschaften]] |volume=88 |issue=1 |pages=37–41 |doi=10.1007/s001140000193 |pmid=11302125 |bibcode=2001NW.....88...37G |s2cid=26608101 |access-date=26 May 2025 }}</ref> However, the uncontrolled application of [[Charring|charred]] waste products of all kinds may endanger soil life and human health.<ref>{{cite journal |last1=Kavitha |first1=Beluri |last2=Pullagurala Venkata Laxma |first2=Reddy |last3=Kim |first3=Bojeong |last4=Lee |first4=Sang Soo |last5=Pandey |first5=Sudhir Kumar |last6=Kim |first6=Ki-Hyun |year=2018 |title=Benefits and limitations of biochar amendment in agricultural soils: a review |url=https://fr.1lib.sk/book/103665148/bf0f82 |journal=[[Journal of Environmental Management]] |volume=227 |pages=146–54 |doi=10.1016/j.jenvman.2018.08.082 |pmid=30176434 |bibcode=2018JEnvM.227..146K |s2cid=52168678 |access-date=26 May 2025 }}</ref>

== History of studies and research ==
The history of the study of soil is intimately tied to humans' urgent need to provide food for themselves and forage for their animals. Throughout history, civilizations have prospered or declined as a function of the availability and productivity of their soils.<ref>{{cite book |last=Hillel |first=Daniel |year=1992 |title=Out of the Earth: civilization and the life of the soil |publisher=[[University of California Press]] |location=Berkeley, California |isbn=978-0-520-08080-5 |url=https://archive.org/details/outofearthcivili0000hill |access-date=26 May 2025 }}</ref>

===Studies of soil fertility===
{{Main|Soil fertility}}
The Greek historian [[Xenophon]] (450–355&nbsp;[[Before the Common Era|BCE]]) was the first to expound upon the merits of green-manuring crops: 'But then whatever weeds are upon the ground, being turned into earth, enrich the soil as much as dung.'{{sfn|Donahue|Miller|Shickluna|1977|p=4}}

[[Columella]]'s ''Of husbandry'', {{circa|60&nbsp;[[Common Era|CE]]}}, advocated the use of lime and that [[clover]] and [[alfalfa]] ([[green manure]]) should be turned under,<ref>{{cite book |last=Columella |first=Lucius Junius Moderatus |year=1745 |title=Of husbandry, in twelve books, and his book concerning trees, with several illustrations from Pliny, Cato, Varro, Palladius, and other antient and modern authors, translated into English |publisher=[[Andrew Millar]] |location=London, United Kingdom |url=https://babel.hathitrust.org/cgi/pt?id=wu.89094198801&seq=7 |access-date=26 May 2025 }}</ref> and was used by 15 generations (450&nbsp;years) under the [[Roman Empire]] until its collapse.{{sfn|Donahue|Miller|Shickluna|1977|p=4}}{{sfn|Kellogg|1957|p=1}} From the [[fall of Rome]] to the [[French Revolution]], knowledge of soil and agriculture was passed on from parent to child and as a result, crop yields were low. During the European [[Middle Ages]], [[Ibn al-'Awwam|Yahya Ibn al-'Awwam]]'s handbook,<ref>{{cite book |language=fr |last=[[Ibn al-'Awwam]] |year=1864 |title=Le livre de l'agriculture, traduit de l'arabe par Jean Jacques Clément-Mullet |series=Filāḥah.French. |publisher=Librairie A. Franck |location=Paris, France |url=https://catalog.hathitrust.org/Record/009953450 |access-date=26 May 2025 }}</ref> with its emphasis on [[irrigation]], guided the people of [[North Africa]], [[Spain]] and the [[Middle East]]; a translation of this work was finally carried to the southwest of the United States when under Spanish influence.<ref>{{cite book |last=Jelinek |first=Lawrence J. |year=1982 |title=Harvest empire: a history of California agriculture |publisher=Boyd and Fraser |location=San Francisco, California |isbn=978-0-87835-131-2 |edition=second |url=https://archive.org/details/harvestempirehis0000jeli/page/n5/mode/2up |access-date=26 May 2025 }}</ref> [[Olivier de Serres]], considered the father of French [[agronomy]], was the first to suggest the abandonment of [[fallowing]] and its replacement by hay [[meadows]] within [[crop rotation]]s. He also highlighted the importance of soil (the French [[terroir]]) in the management of [[vineyard]]s. His famous book {{Lang|fr|Le Théâtre d'Agriculture et mesnage des champs}}<ref>{{cite book |language=fr |last=de Serres |first=Olivier |year=1600 |title=Le Théâtre d'Agriculture et mesnage des champs |publisher=Jamet Métayer |location=Paris, France |url=https://gallica.bnf.fr/ark:/12148/bpt6k738381/f1.image |access-date=26 May 2025 }}</ref> contributed to the rise of modern, [[sustainable agriculture]] and to the collapse of old [[agricultural practices]] such as [[soil amendment]] for crops by the lifting of [[forest litter]] and [[assarting]], which ruined the soils of western Europe during the [[Middle Ages]] and even later on according to regions.<ref>{{cite journal |last1=Virto |first1=Iñigo |last2=Imaz |first2=María José |last3=Fernández-Ugalde |first3=Oihane |last4=Gartzia-Bengoetxea |first4=Nahia |last5=Enrique |first5=Alberto |last6=Bescansa |first6=Paloma |journal=[[Sustainability (journal)|Sustainability]] |volume=7 |issue=1 |title=Soil degradation and soil quality in western Europe: current situation and future perspectives |year=2015 |pages=313–65 |doi=10.3390/su7010313 |doi-access=free |hdl=2454/26163 |hdl-access=free }}</ref>

Experiments into what made plants grow first led to the idea that the ash left behind when plant matter was burned was the essential element but overlooked the role of nitrogen, which is not left on the ground after combustion, a belief which prevailed until the 19th century.<ref>{{cite journal |last1=Van der Ploeg |first1=Rienk R. |last2=Schweigert |first2=Peter |last3=Bachmann |first3=Joerg |journal=[[Scientific World Journal]] |volume=1 |issue=S2 |title=Use and misuse of nitrogen in agriculture: the German story |year=2001 |pages=737–44 |doi=10.1100/tsw.2001.263 |pmid=12805882 |pmc=6084271 |doi-access=free }}</ref> In about 1635, the Flemish chemist [[Jan Baptist van Helmont]] thought he had proved water to be the essential element from his famous five years' experiment with a willow tree grown with only the addition of rainwater. His conclusion came from the fact that the increase in the plant's weight had apparently been produced only by the addition of water, with no reduction in the soil's weight.<ref>{{cite web |url=https://www.bbc.co.uk/bitesize/watch/zpgb4wx |title=Van Helmont's experiments on plant growth |website=[[BBC World Service]] |access-date=27 May 2025 }}</ref><ref name=Brady1984/>{{sfn|Kellogg|1957|p=3}} [[John Woodward (naturalist)|John Woodward]] ({{abbr|d.|died}}&nbsp;1728) experimented with various types of water ranging from clean to muddy and found muddy water the best, and so he concluded that earthy matter was the essential element. Others concluded it was humus in the soil that passed some essence to the growing plant. Still others held that the vital growth principal was something passed from dead plants or animals to the new plants. At the start of the 18th century, [[Jethro Tull (agriculturist)|Jethro Tull]] demonstrated that it was beneficial to cultivate (stir) the soil, but his opinion that the stirring made the fine parts of soil available for plant absorption was erroneous.<ref name=Brady1984/>{{sfn|Kellogg|1957|p=2}}

As chemistry developed, it was applied to the investigation of soil fertility. The French chemist [[Antoine Lavoisier]] showed in about 1778 that plants and animals must [[Combustion|combust]] oxygen internally to live. He was able to deduce that most of the {{convert|165|lb|adj=on}} weight of Van Helmont's willow tree derived from air.<ref>{{cite journal |language=fr |last=de Lavoisier |first=Antoine-Laurent |journal=Mémoires de l'Académie Royale des Sciences |title=Mémoire sur la combustion en général |year=1777 |url=https://www.academie-sciences.fr/pdf/dossiers/Franklin/Franklin_pdf/Mem1777_p592.pdf |access-date=27 May 2025 }}</ref> It was the French agriculturalist [[Jean-Baptiste Boussingault]] who by means of experimentation obtained evidence showing that the main sources of carbon, hydrogen and oxygen for plants were air and water, while nitrogen was taken from soil.<ref>{{cite book |language=fr |last=Boussingault |first=Jean-Baptiste |title=Agronomie, chimie agricole et physiologie, volumes 1–5 |year=1860–1874 |publisher=Mallet-Bachelier |location=Paris, France |url=https://archive.org/details/8TSUP364_1 |access-date=27 May 2025 }}</ref> [[Justus von Liebig]] in his book ''Organic chemistry in its applications to agriculture and physiology'' (published 1840), asserted that the chemicals in plants must have come from the soil and air and that to maintain soil fertility, the used minerals must be replaced.<ref>{{cite book |last=von Liebig |first=Justus |title=Organic chemistry in its applications to agriculture and physiology |year=1840 |publisher=Taylor and Walton |location=London, United Kingdom |url=https://archive.org/details/organicchemistry00liebrich |access-date=27 May 2025 }}</ref> Liebig nevertheless believed the nitrogen was supplied from the air. The enrichment of soil with guano by the Incas was rediscovered in 1802, by [[Alexander von Humboldt]]. This led to its mining and that of Chilean nitrate and to its application to soil in the United States and Europe after 1840.<ref>{{cite journal |last=Way |first=J. Thomas |journal=Journal of the Royal Agricultural Society of England |title=On the composition and money value of the different varieties of guano |year=1849 |volume=10 |pages=196–230 |url=https://www.biodiversitylibrary.org/item/37078#page/220/mode/1up |access-date=27 May 2025 }}</ref>

The work of Liebig was a revolution for agriculture, and so other investigators started experimentation based on it. In England [[John Bennet Lawes]] and [[Joseph Henry Gilbert]] worked in the [[Rothamsted Research|Rothamsted Experimental Station]], founded by the former, and {{Not a typo|(re)discovered}} that plants took nitrogen from the soil, and that salts needed to be in an available state to be absorbed by plants. Their investigations also produced the [[superphosphate]], consisting in the acid treatment of phosphate rock.{{sfn|Kellogg|1957|p=4}} This led to the invention and use of salts of potassium (K) and nitrogen (N) as [[fertilizer]]s. Ammonia generated by the production of [[coke (fuel)|coke]] was recovered and used as fertiliser.<ref>{{cite web |last=Tandon |first=Hari L.S. |url=http://www.tandontech.net/fertilisers.html |title=A short history of fertilisers |website=Fertiliser Development and Consultation Organisation |access-date=17 December 2017 |archive-url=https://web.archive.org/web/20170123214241/http://www.tandontech.net/fertilisers.html |archive-date=23 January 2017 }}</ref> Finally, the chemical basis of nutrients delivered to the soil in manure was understood and in the mid-19th century chemical fertilisers were applied. However, the dynamic interaction of soil and its life forms was still not understood.

In 1856, J. Thomas Way discovered that ammonia contained in fertilisers was transformed into [[nitrate]],<ref>{{cite journal |last=Way |first=J. Thomas |journal=Journal of the Royal Agricultural Society of England |title=On the power of soils to absorb manure |year=1852 |volume=13 |pages=123–43 |url=https://biodiversitylibrary.org/page/45583402 |access-date=27 May 2025 }}</ref> and twenty years later [[Robert Warington]] proved that this transformation was done by living organisms.<ref>{{cite book |last=Warington |first=Robert |title=Note on the appearance of nitrous acid during the evaporation of water: a report of experiments made in the Rothamsted laboratory |url=https://books.google.com/books?id=NlISAQAAMAAJ |year=1878 |publisher=[[Harrison and Sons]] |location=London, United Kingdom |access-date=27 May 2025 }}</ref> In 1890 [[Sergei Winogradsky]] announced he had found the bacteria responsible for this transformation.<ref>{{cite journal |last=Winogradsky |first=Sergei |journal=[[Comptes Rendus de l'Académie des Sciences|Comptes Rendus Hebdomadaires des Séances de l'Académie des Sciences]] |title=Sur les organismes de la nitrification |language=fr |trans-title=On the organisms of nitrification |year=1890 |volume=110 |issue=1 |pages=1013–16 |url=https://gallica.bnf.fr/ark:/12148/bpt6k30663/f1087.item |access-date=27 May 2025 }}</ref>

It was known that certain [[legume]]s could take up nitrogen from the air and fix it to the soil but it took the development of bacteriology towards the end of the 19th century to lead to an understanding of the role played in nitrogen fixation by bacteria. The symbiosis of bacteria and leguminous roots, and the fixation of nitrogen by the bacteria, were simultaneously discovered by the German agronomist [[Hermann Hellriegel]] and the Dutch microbiologist [[Martinus Beijerinck]].{{sfn|Kellogg|1957|p=4}}

Crop rotation, mechanisation, chemical and natural fertilisers led to a doubling of wheat yields in western Europe between 1800 and 1900.{{sfn|Kellogg|1957|pp=1–4}}

===Studies of soil formation===
{{See also|Soil formation}}
Scientists who studied soil in connection with agricultural practices considered it mainly a static substrate. However, the soil is the result of evolution from more ancient geological materials under the action of biotic and abiotic processes. After studies of soil improvement commenced, other researchers began to study soil genesis and, as a result, soil types and classifications.

In 1860, while in Mississippi, [[Eugene W. Hilgard]] (1833–1916) studied the relationship between rock material, climate, vegetation, and the type of soils that were developed. He realised that the soils were dynamic and considered the classification of soil types.<ref>{{cite book |last=Hilgard |first=Eugene W. |title=Soils: their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions |year=1907 |publisher=[[The Macmillan Company]] |location=London, United Kingdom |url=https://www.biodiversitylibrary.org/item/65783#page/9/mode/1up |access-date=27 May 2025 }}</ref> His work was not continued. At about the same time, [[Friedrich Albert Fallou]] described soil profiles and related soil characteristics to their formation as part of his professional work evaluating forest and farmland for the principality of [[Saxony]]. His 1857 book, {{Lang|de|Anfangsgründe der Bodenkunde}} (First principles of soil science), established modern soil science.<ref>{{cite book |language=de |last=Fallou |first=Friedrich Albert |title=Anfangsgründe der Bodenkunde |year=1857 |publisher=G. Schönfeld's Buchhandlung |location= Dresden, Germany |url=https://play.google.com/store/books/details?id=XtE0f3l8_T8C&rdid=book-XtE0f3l8_T8C&rdot=1 |access-date=27 May 2025 |archive-url=https://web.archive.org/web/20181215223343/http://digital.slub-dresden.de/fileadmin/data/321768043/321768043_tif/jpegs/321768043.pdf |archive-date=15 December 2018 |url-status=live }}</ref> Contemporary with Fallou's work, and driven by the same need to accurately assess land for equitable taxation, [[Vasily Dokuchaev]] led a team of soil scientists in Russia who conducted an extensive survey of soils, observing that similar basic rocks, climate and vegetation types lead to similar soil layering and types, and established the concepts for soil classifications. Due to language barriers, the work of this team was not communicated to Western Europe until 1914 through a publication in German by [[Konstantin Glinka]], a member of the Russian team.<ref>{{cite book |language=de |last=Glinka |first=Konstantin Dmitrievich |title=Die Typen der Bodenbildung: ihre Klassifikation und geographische Verbreitung |year=1914 |publisher=[[Borntraeger]] |location=Berlin, Germany }}</ref>

[[Curtis F. Marbut]], influenced by the work of the Russian team, translated Glinka's publication into English,<ref>{{cite book |last=Glinka |first=Konstantin Dmitrievich |title=The great soil groups of the world and their development |url=https://reader.library.cornell.edu/docviewer/digital?id=chla3055800#mode/1up |year=1927 |publisher=Edwards Brothers |location=Ann Arbor, Michigan |access-date=27 May 2025 }}</ref> and, as he was placed in charge of the U.S. [[National Cooperative Soil Survey]], applied it to a national soil classification system.<ref name=Brady1984/>

==See also==
{{portal|Environment|Geology}}
{{div col|content=
*[[Acid sulfate soil]]
*[[Agricultural science]]
*[[Agrophysics]]
*[[Crust (geology)|Crust]]
*[[Factors affecting permeability of soils]]
*[[Geomorphology]]
*[[Index of soil-related articles]]
*[[Lunar soil]] and [[martian soil]]
*[[Mycorrhizal fungi and soil carbon storage]]
*[[Red soil]]
*[[Shrink–swell capacity]]
*[[Soil biodiversity]]
*[[Soil liquefaction]]
*[[Soil moisture velocity equation]]
*[[Soil zoology]]
*[[Tillage erosion]]
*[[World Soil Museum]]

}}

== References ==
{{reflist}}

==Sources==
{{Free-content attribution
| title = Drowning in Plastics – Marine Litter and Plastic Waste Vital Graphics
| publisher = United Nations Environment Programme
| documentURL = https://www.unep.org/resources/report/drowning-plastics-marine-litter-and-plastic-waste-vital-graphics
| license statement URL = https://commons.wikimedia.org/wiki/File:United_Nations_Environment_Programme_Drowning_in_Plastics_%E2%80%93_Marine_Litter_and_Plastic_Waste_Vital_Graphics.pdf
| license = Cc BY-SA 3.0 IGO
}}

==Bibliography==
{{refbegin}}
*{{cite book |last1=Donahue |first1=Roy Luther |title=Soils: An Introduction to Soils and Plant Growth |last2=Miller |first2=Raymond W. |last3=Shickluna |first3=John C. |year=1977 |publisher=[[Prentice-Hall]] |isbn=978-0-13-821918-5 |url=https://archive.org/details/soilsintroductio00dona}}
*{{cite web |title=Arizona Master Gardener |url=http://ag.arizona.edu/pubs/garden/mg/soils/soils.html|publisher=Cooperative Extension, College of Agriculture, [[University of Arizona]]  |access-date=27 May 2013}}
*{{cite book |editor-last=Stefferud |editor-first=Alfred |title=Soil: The Yearbook of Agriculture 1957 |year=1957 |publisher=United States Department of Agriculture |url=https://archive.org/stream/yoa1957#page/n18/mode/1up |oclc=704186906}}
**{{harvc |name-list-style=harv |last=Kellogg |first=Charles E. |chapter=We Seek; We Learn |in=Stefferud |year=1957 |url=//archive.org/stream/yoa1957#page/n17/mode/1up}}
**{{harvc |name-list-style=harv |last=Simonson |first=Roy W. |chapter=What Soils Are |in=Stefferud |year=1957 |url=//archive.org/stream/yoa1957#page/n34/mode/1up}}
**{{harvc |name-list-style=harv |last=Russell |first=M.B. |chapter=Physical Properties |in=Stefferud |year=1957 |url=//archive.org/stream/yoa1957#page/n49/mode/1up}}
**{{harvc |name-list-style=harv |last=Dean |first=L.A. |chapter=Plant Nutrition and Soil Fertility |in=Stefferud |year=1957 |url=//archive.org/stream/yoa1957#page/n100/mode/1up}}
**{{harvc |name-list-style=harv |last=Russel |first=Darrell A. |chapter=Boron and Soil Fertility |in=Stefferud |year=1957 |url=//archive.org/stream/yoa1957#page/n145/mode/1up |oclc=704186906}}

{{refend}}

==Further reading==
{{refbegin|colwidth=33em}}
*[http://www.soil-net.com/ Soil-Net.com] {{Webarchive|url=https://web.archive.org/web/20080710061716/http://www.soil-net.com/ |date=10 July 2008 }} A free schools-age educational site teaching about soil and its importance.
*Adams, J.A. 1986. ''Dirt''. College Station, Texas: Texas A&M University Press {{ISBN|0-89096-301-0}}
*Certini, G., Scalenghe, R. 2006. Soils: Basic concepts and future challenges. Cambridge Univ Press, Cambridge.
*[[David R. Montgomery|Montgomery, David R.]], ''Dirt: The Erosion of Civilizations'' (U of California Press, 2007), {{ISBN|978-0-520-25806-8}}
*Faulkner, Edward H. ''Plowman's Folly'' (New York, Grosset & Dunlap, 1943). {{ISBN|0-933280-51-3}}
*[https://web.archive.org/web/20080705133103/http://www.landis.org.uk/soilscapes LandIS Free Soilscapes Viewer] Free interactive viewer for the Soils of England and Wales
*Jenny, Hans. 1941. [https://web.archive.org/web/20130225050838/http://soilandhealth.org/01aglibrary/010159.Jenny.pdf Factors of Soil Formation: A System of Quantitative Pedology]
*Logan, W.B. ''Dirt: The ecstatic skin of the earth'' (1995). {{ISBN|1-57322-004-3}}
*Mann, Charles C. September 2008. " Our good earth" ''National Geographic Magazine''

==External links==
*{{cite web|url=http://www.mvm.usace.army.mil/Readiness/97flood/flood.htm |title=97 Flood |publisher=USGS |access-date=8 July 2008 |archive-url=https://web.archive.org/web/20080624040143/http://www.mvm.usace.army.mil/Readiness/97flood/flood.htm |archive-date=24 June 2008}} Photographs of sand boils.
*Soil Survey Division Staff. 1999. ''Soil survey manual''. Soil Conservation Service. U.S. Department of Agriculture Handbook 18.
*Soil Survey Staff. 1975. ''Soil Taxonomy: A basic system of soil classification for making and interpreting soil surveys.'' USDA-SCS Agric. Handb. 436. United States Government Printing Office, Washington, DC.
*[https://web.archive.org/web/20060828063956/http://forages.oregonstate.edu/is/ssis/main.cfm?PageID=3 Soils (Matching suitable forage species to soil type)], Oregon State University
*{{cite web|url= http://jan.ucc.nau.edu/~doetqp-p/courses/env320/lec1/Lec1.html|title= Lecture 1 Chapter 1 Why Study Soils?|access-date= 7 January 2019|last= Gardiner|first= Duane T|website= ENV320: Soil Science Lecture Notes|publisher= Texas A&M University-Kingsville|archive-url= https://web.archive.org/web/20180209052922/http://jan.ucc.nau.edu/~doetqp-p/courses/env320/lec1/Lec1.html|archive-date= 9 February 2018}}
*Janick, Jules. 2002. [https://web.archive.org/web/20050317030248/http://www.hort.purdue.edu/newcrop/tropical/lecture_06/chapter_12l_R.html Soil notes], Purdue University
*[http://www.landis.org.uk/ LandIS Soils Data for England and Wales] {{Webarchive|url=https://web.archive.org/web/20070716033248/http://www.landis.org.uk/ |date=16 July 2007 }} a pay source for GIS data on the soils of England and Wales and soils data source; they charge a handling fee to researchers.
{{refend}}

{{wiktionary|soil}}
{{wikiversity|Soil Formation}}
{{Wikibooks |Historical Geology|Soils and paleosols}}
{{Commons category|Soils}}
{{Wikiquote}}
{{div col|content=
*[https://www.theguardian.com/environment/video/2019/jul/11/its-time-we-stopped-treating-soil-like-dirt-video Short video explaining soil basics]
*[http://www.edaphic.com.au/soil-water-compendium/ The Soil Water Compendium (soil water content sensors explained)]
*[http://www.fao.org/globalsoilpartnership/en/ Global Soil Partnership]
*[http://www.fao.org/soils-portal/en/ FAO Soils Portal]
*[https://wrb.isric.org/ World Reference Base for Soil Resources]
*[https://www.isric.org/ ISRIC – World Soil Information (ISC World Data Centre for Soils)]
*[https://www.isric.org/explore/library ISRIC -World Soil Library and Maps]
*[https://wsm.isric.org/ ISRIC - World Soil Museum (WSM virtual)]
*[https://data.isric.org/ ISRIC - Soil data hub]
*[http://www.wossac.com/ Wossac the world soil survey archive and catalogue]
*[http://csss.ca/ Canadian Society of Soil Science]
*[https://www.soils.org/ Soil Science Society of America]
*[https://websoilsurvey.nrcs.usda.gov/app/HomePage.htm USDA-NRCS Web Soil Survey]
*[http://eusoils.jrc.ec.europa.eu/ European Soil Portal] (wiki)
*[http://www.cranfield.ac.uk/sas/nsri National Soil Resources Institute UK]
*[http://passel.unl.edu/ Plant and Soil Sciences eLibrary]
*[https://archive.org/details/yoa1957 Copies of the reference 'Soil: The Yearbook of Agriculture 1957' in multiple formats]
}}

{{Use dmy dates|date=June 2019}}
{{Soil science topics}}
{{Geotechnical engineering}}
{{Natural resources}}
{{Authority control}}

[[Category:Soil| ]]
[[Category:Land management]]
[[Category:Horticulture]]
[[Category:Granularity of materials]]
[[Category:Natural materials]]
[[Category:Natural resources]]