The
Mpemba effect is the observation that, in certain specific circumstances, warmer
water freezes faster than colder water.
New Scientist recommends starting the experiment with containers at 35°C and 5°C to maximise the effect.
Origin
The effect is named for the
Tanzanian high-school student Erasto B. Mpemba. Mpemba first encountered the phenomenon in 1963 in Form 3 of Magamba Secondary School, Tanzania when freezing hot
ice cream mix in cookery classes and noticing that they froze before cold mixes. After passing his
O-level examinations, he became a student at Mkwawa Secondary (formerly High) School,
Iringa,
Tanzania. The headmaster invited Dr.
Denis G. Osborne from the University College in
Dar Es Salaam to give a lecture on
physics. After the lecture, Erasto Mpemba asked him the question "If you take two similar containers with equal volumes of water, one at 35°C and the other at 100°C, and put them into a freezer, the one that started at 100°C freezes first. Why?" only to be ridiculed by his classmates and teacher. After initial consternation, Dr. Osborne confirmed Erasto's finding and they published the results together in 1969. Erasto Mpemba currently works for the
African Forestry and Wildlife Commission.
Causes
At first sight, the behaviour seems contrary to
thermodynamics. However, the Mpemba effect can be explained with standard physical theory. Many effects can contribute to the observation, depending on the experimental set-up:
- Definition of frozen: Is it the physical definition of the point at which water forms a visible surface layer of ice, or the point at which the entire volume of water becomes a solid block of ice?
- Evaporation: Reducing the volume to be frozen. Evaporation is endothermic.
- Convection: Accelerating heat transfers. Reduction of water density below 4°C tends to suppress the convection currents cooling the lower part of the liquid mass; the lower density of hot water would reduce this effect, perhaps sustaining the more rapid initial cooling.
- Frost: Has insulating effects. The lower temperature water will tend to freeze from the top, reducing further heat loss by radiation and air convection, while the warmer water will tend to freeze from the bottom and sides because of water convection. This is disputed as there are experiments which account for this factor.
- Supercooling: It is hypothesized that cold water, when placed in a freezing environment, supercools more than hot water in the same environment, thus solidifying slower than hot water. However, supercooling tends to be less significant where there are particles that act as nuclei for ice crystals, thus precipitating rapid freezing.
- Solutes: The effects of calcium, magnesium carbonate among others.
- The effect of heating on dissolved gases.
Scalar functionality
According to an article by Monwhea Jeng: "Analysis of the situation is now quite complex, since we are no longer considering a single parameter, but a scalar function, and
computational fluid dynamics (CFD) is notoriously difficult."
This effect is a heat transfer problem, and therefore well suited to be studied from a transport phenomena viewpoint, based on continuum mechanics. When heat transfer is analyzed in terms of partial differential equations, whose solutions depend on a number of conditions, it becomes clear that measuring only a few lumped parameters, such as the water average temperature is generally insufficient to define the system behaviour, since conditions such as geometry, fluid properties and temperature and flow fields play an important role. The counterintuitiveness of the effect, if analyzed only in terms of simplified thermodynamics illustrates the need to include all the relevant variables and use the best available theoretical tools when approaching a physical problem.
Recent view of the Mpemba effect
A reviewer for
Physics World writes, "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.
Historical observations
Similar behavior may have been observed by ancient scientists such as
Aristotle, and
Early Modern scientists such as
Francis Bacon and
René Descartes. Aristotle's explanation involved an erroneous property he called
antiperistasis, defined as "the supposed increase in the intensity of a quality as a result of being surrounded by its contrary quality".
References
Bibliography
External links