Mpemba effect

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Template:Short description The Mpemba effect is the observation that hot liquids or colloids (such as ice cream) can freeze more quickly than colder ones, for similar volumes and surrounding conditions. Physicists remain divided on the effect's reproducibility, precise definition, and underlying mechanisms.<ref>Template:Cite web</ref> It is named after Erasto Mpemba, a Tanzanian teenager who studied it scientifically in the 1960s for the first time, along with Denis Osborne.<ref>Aristotle in E. W. Webster, Meteorologica I, Oxford: Oxford University Press, 1923, pp. 348b–349a. "The fact that water has previously been warmed contributes to its freezing quickly; for so it cools sooner. Hence many people, when they want to cool hot water quickly, begin by putting it in the sun."</ref>

The Mpemba effect was initially observed in ice cream and water, and later in other colloids.<ref name=":1">Template:Cite journal</ref><ref name=":5">Template:Citation</ref><ref>Template:Citation</ref> It has been studied extensively in water, with mixed results, and some experiments finding no reproducible effect.<ref name="Tao">Template:Cite journal</ref> It has also been studied in magnetic alloys, nanomechanical systems,<ref>Template:Cite journal</ref> and quantum systems.<ref>Template:Citation</ref><ref name=":2">Template:Cite journal</ref><ref name=":3">Template:Cite web</ref>

Definition

The definition of the Mpemba effect used in theoretical studies varies,<ref name="arxiv.org" /> making it difficult to compare experiments.<ref name="ball">Template:Cite web</ref> Monwhea Jeng proposed this definition for the effect in water: "There exists a set of initial parameters, and a pair of temperatures, such that given two bodies of water identical in these parameters, and differing only in initial uniform temperatures, the hot one will freeze sooner."<ref name="Jeng">Template:Cite journal</ref> Even this definition does not specify whether "freezing" refers to the point at which a visible surface layer of ice has formed, or the point at which the liquid is completely frozen.<ref name="ball" />

A generalized definition is "When a hotter system equilibrates faster than a colder one when both are quenched to the same low temperature."<ref name=":6">Template:Cite journal</ref> In water, this would be when the liquid has completely frozen.

Mpemba's observation

The effect is named after Tanzanian student Erasto Mpemba, who described it in 1963 in Form 3 of Magamba Secondary School, Tanganyika; when freezing a hot ice cream mixture in a cookery class, he noticed that it froze before a cold mixture. He later became a student at Mkwawa Secondary (formerly High) School in Iringa. The headmaster invited Dr. Denis Osborne from the University College in Dar es Salaam to give a lecture on physics. After the lecture, Mpemba asked him, "If you take two similar containers with equal volumes of water, one at Template:Convert and the other at Template:Convert, and put them into a freezer, the one that started at Template:Convert freezes first. Why?" When Osborne experimented on the issue back at his workplace, he confirmed Mpemba's finding. They later published the results together in 1969, while Mpemba was studying at the College of African Wildlife Management.<ref name="Mpemba">Template:Cite journal republished as Template:Cite journal</ref>

Mpemba and Osborne described placing Template:Convert samples of water in Template:Convert beakers in the icebox of a domestic refrigerator on a sheet of polystyrene foam. They showed the time for freezing to start was longest with an initial temperature of Template:Convert and that it was much less at around Template:Convert. They ruled out loss of liquid volume by evaporation and the effect of dissolved air as significant factors. In their setup, most heat loss was found to be from the liquid surface.<ref name="Mpemba" />

History

Various effects of heat on the freezing of water were described by ancient scientists, including Aristotle: "The fact that the water has previously been warmed contributes to its freezing quickly: for so it cools sooner. Hence many people, when they want to cool water quickly, begin by putting it in the sun."<ref>Template:Cite web</ref> Aristotle's explanation involved antiperistasis: "...the supposed increase in the intensity of a quality as a result of being surrounded by its contrary quality."Template:Citation needed

Francis Bacon noted that "slightly tepid water freezes more easily than that which is utterly cold."<ref>Bacon, Francis; Novum Organum, Lib. II, L. In the original Latin: "Aqua parum tepida facilius conglacietur quam omnino frigida."</ref> René Descartes wrote in his Discourse on the Method, relating the phenomenon to his vortex theory: "One can see by experience that water that has been kept on a fire for a long time freezes faster than other, the reason being that those of its particles that are least able to stop bending evaporate while the water is being heated."<ref>Template:Cite web</ref>

Scottish scientist Joseph Black in 1775 investigated a special case of the phenomenon by comparing previously boiled with unboiled water.<ref>Template:Cite journal</ref> He found that the previously boiled water froze more quickly, even when evaporation was controlled for. He discussed the influence of stirring on the results of the experiment, noting that stirring the unboiled water led to it freezing at the same time as the previously boiled water, and also noted that stirring the very-cold unboiled water led to immediate freezing. Joseph Black then discussed Daniel Gabriel Fahrenheit's description of supercooling of water, arguing that the previously boiled water could not be as readily supercooled.Template:Citation needed

Modern experimental work

Studies of the effect in water

Modern studies using freezers with well-understood properties have observed the Mpemba effect where water supercools before freezing. Water that starts out cooler tends to reach a lower supercooled temperature before freezing. Some studies measure the time it takes for a sample to begin to freeze (the start of recalescence, the moment where the heat of freezing first starts to be released) the time it takes to completely freeze, or the difference: the time from the onset of recalescence to the completion of freezing. Some also measure the time it takes for a sample to reach the freezing point of the fluid, before any freezing has begun.

In 1995, David Auerbach studied glass beakers placed into a liquid cooling bath, where the water supercooled to Template:Convert before freezing. In some cases water which started off hotter began freezing first.<ref>Template:Cite journal</ref> Considerable random variation was observed in the time required for spontaneous freezing to start, and Auerbach observed the Mpemba effect more frequently when the ambient temperature was between –6 and Template:Convert. James Brownridge later studied a variety of initial conditions and containers, measuring the time to the onset of recalescence, and found that while hot samples sometimes froze first this was also affected by properties of the container holding the liquid.<ref name="Brownridge 2011">Template:Cite journal</ref>

Writing for New Scientist, Mick O'Hare recommended starting the experiment with containers at Template:Convert, respectively, to maximize the effect.<ref>How to Fossilize Your Hamster: And Other Amazing Experiments for the Armchair Scientist, Template:ISBN</ref>

In 2021, John Bechhoefer described a way to reliably reproduce the effect.<ref>Template:Cite journal</ref> In 2024, Argelia Ortega, et al. studied the freezing of small (1-20mL) drops in a Peltier cell with a thermographic camera, and found that hot drops consistently froze faster than cold ones, with a more pronounced difference for larger drops. In particular, hot drops finished freezing sooner after the onset of recalescence, and experienced less of a temperature spike during the freezing process.<ref name=":4">Template:Cite journal</ref>

Criticisms of experiments with water

Some researchers have criticized studies of the Mpemba effect for not accounting for dissolved solids and gasses, and other confounding factors.<ref name="arxiv.org">Template:Cite book</ref> Even among experiments that agree on a definition and observe the Mpemba effect for some experimental setups, they often do not observe it for all setups and starting conditions.<ref name="ball" />

In 2006, Philip Ball, a reviewer for Physics World wrote: "Even if the Mpemba effect is real — if hot water can sometimes freeze more quickly than cold — it is not clear whether the explanation would be trivial or illuminating."<ref name="ball" /> Ball wrote that investigations of the phenomenon need to control a large number of initial parameters (including type and initial temperature of the water, dissolved gas and other impurities, and size, shape and material of the container, the method of cooling, and the temperature of the refrigerator) and the need to settle on a particular method of establishing the time of freezing. Ball described simple ways in which the effect might be observed, such as if a warmer temperature melts the frost on a cooling surface, thereby increasing thermal conductivity between the cooling surface and the water container.<ref name="ball" />

In 2016, Burridge and Linden studied a slightly different measure, the time it took water samples to reach 0 °C but not freeze. They carried out their own experiments, and reviewed previous work by others. Their review noted that the large effects observed in early experiments had not been replicated in other studies of cooling to the freezing point, and that studies showing small effects could be influenced by variations in the positioning of thermometers: "We conclude, somewhat sadly, that there is no evidence to support meaningful observations of the Mpemba effect."<ref name="Burridge">Template:Cite journal</ref>

Studies of the effect in colloids and other systems

Classical systems

The original classroom observations of the Mpemba effect were of fresh ice cream, a colloid, freezing in a freezer.

A generalized version of the Mpemba effect is "when a hotter system equilibrates faster than a colder one when both are quenched to the same low temperature." This has been modeled theoretically for simple systems such as single particles under Brownian motion.<ref name=":6" />

The possibility of a "strong Mpemba effect" where exponentially faster cooling can occur in a system at particular initial temperatures was predicted in 2019 by Klich, Raz, Hirschberg and Vucelja. If they existed, the effect in such systems would be easy to observe experimentally.<ref>Template:Cite journal</ref> In 2020 the strong Mpemba effect was demonstrated experimentally by Avinash Kumar and John Boechhoefer in a single-particle colloidal system.<ref name=":1" /> In 2022, that group also demonstrated an "inverse Mpemba effect" in a single-particle colloid where a cold system heats up much faster than a warmer one, under the right conditions.<ref>Template:Cite journal</ref>

Quantum systems

Since 2020, quantum researchers have studied Mpemba effects in quantum systems as an example of how initial conditions of a system affects its thermal evolution. In 2024, a team in John Goold's lab at Trinity College described their quantum-mechanical analysis of an abstract problem wherein "an initially hot system is quenched into a cold bath and reaches equilibrium faster than an initially cooler system."<ref name=":2" /> They included computational studies of spin systems which exhibit the effect,<ref name=":2" /> concluding that certain initial conditions of a quantum system can lead to a simultaneous increase in the thermalization rate and the free energy.<ref name=":3" />

In 2025, experimental observations by Zhang, et al. found a quantum strong Mpemba effect for a single trapped ion,<ref>Template:Cite journal</ref> and Chatterjee, et al. found the Mpemba effect occurs naturally during the cooling of nuclear spin states.<ref>Template:Citation</ref>

Theoretical explanations

While the definition of the Mpemba effect used in theoretical studies varies,<ref name="arxiv.org" /> several explanations have been offered for its occurrence.

In 2017, two research groups independently and simultaneously found a theoretical Mpemba effect and also predicted a new "inverse" Mpemba effect in which heating a cooled, far-from-equilibrium system takes less time than another system that is initially closer to equilibrium. Zhiyue Lu and Oren Raz yielded a general criterion based on Markovian statistical mechanics, predicting the appearance of the inverse Mpemba effect in the Ising model and diffusion dynamics.<ref>Template:Cite journal</ref> Antonio Lasanta and co-authors also predicted the direct and inverse Mpemba effects for a granular gas in a far-from-equilibrium initial state.<ref name=":0">Template:Cite journal</ref> Lasanta's paper also suggested that a very generic mechanism leading to both Mpemba effects is due to a particle velocity distribution function that significantly deviates from the Maxwell–Boltzmann distribution.<ref name=":0" />

In 2024, building on Kumar's work, Isha Malhotra simulated single colloids placed in a different, double-well potential, and predicted conditions under which two specific ranges of hotter starting temperatures lead to faster freezing, but not temperatures in between those ranges.<ref name=":5" />

Supercooling is a component of many theoretical explanations, particularly the tendency of hot liquids that are cooled rapidly to start freezing at a higher supercool temperature.<ref>Template:Cite news</ref><ref name="Brownridge 2011" /> Several molecular dynamics simulations have also supported that changes in hydrogen bonding during supercooling play a role in the process.<ref name="Jin" /><ref name="Sun">Template:Cite journal</ref> In 2017, Yunwen Tao and co-authors suggested that the vast diversity and peculiar occurrence of different hydrogen bonds could contribute to the effect. They argued that the number of strong hydrogen bonds increases as temperature is elevated, and that the existence of the small strongly bonded clusters facilitates in turn the nucleation of hexagonal ice when warm water is rapidly cooled down. The authors used vibrational spectroscopy and modelling with density functional theory-optimized water clusters.<ref name="Tao" />

The following additional explanations have been proposed:

  • Solutes: Calcium carbonate, magnesium carbonate, and other mineral salts dissolved in water can precipitate out when water is boiled, leading to an increase in the freezing point compared to non-boiled water that contains all the dissolved minerals.<ref>Template:Cite journal</ref>
  • Dissolved gases: Cold water can contain more dissolved gases than hot water, which may somehow change the properties of the water with respect to convection currents.<ref name="Jeng" />
  • Microbubble-induced heat transfer: Boiling may induce microbubbles in water that remain stably suspended as the water cools, then act by convection to transfer heat more quickly as the water cools.<ref>Template:Cite journal</ref><ref>Template:Cite news</ref>
  • Convection, accelerating heat transfers: Reduction of water density below Template:Convert tends to suppress the convection currents that cool the lower part of the liquid mass; the lower density of hot water would reduce this effect, perhaps sustaining the more rapid initial cooling. Higher convection in the warmer water may also spread ice crystals around faster.<ref>CITV Prove It! Series 1 Programme 13 Template:Webarchive</ref> Colder temperature may freeze more readily from the top, reducing further heat loss by radiation and air convection; while warmer water freezes from the bottom and sides because of water convection. Some experiments account for this factor.<ref name="Jeng" />
  • Frost: Frost has insulating effects. A container of hotter liquid may melt through a layer of frost that is acting as an insulator around a cooler container, allowing the container to work more effectively within the same refrigeration setup.<ref name="Brownridge 2011" />
  • Crystallization: A relatively higher population of water hexamer states in warm water might be responsible for the faster crystallization.<ref name="Jin">Template:Cite journal</ref>
  • Distribution function: Strong deviations from the Maxwell–Boltzmann distribution can result in a Mpemba effect in gases and granular fluids.<ref name=":0" />

Andrei A. Klimov and Alexei V. Finkelstein state that there is a great variability in freezing speed, explaining the Mpemba effect as of stochastic origin.<ref>The Mpemba Effect in Pure Water Has a Stochastic Origin. Experimental and Theoretical Resolution of the Paradox [1] </ref>

See also

References

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