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Mancosu - Philosophy of Mathematical Practice (Oxford, 2008).pdf

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the boundary between mathematics and physics 409defined critical temperature at which a phase transition takes place. If we turnthe external field <strong>of</strong>f above the critical temperature, the material no longerexhibits magnetic properties. However, if we turn it <strong>of</strong>f below the criticaltemperature, the material retains a residual magnetic field, a phenomenoncalled ‘spontaneous magnetization’.Spontaneous magnetization appears as a collective property <strong>of</strong> large numbers<strong>of</strong> ferromagnetic atoms. Although the physical property presumably arises fromthe interaction <strong>of</strong> individual atoms, Pierre Weiss (1907) proposed the simplifiedmodel <strong>of</strong> a ‘molecular field’ representing the magnetic force η produced by thecollection <strong>of</strong> atoms and postulated the self-consistent equation η = tanh(η/T ),where T is a variable representing the temperature. This simple and primitivepicture, the most elementary example <strong>of</strong> the class <strong>of</strong> mean field models, in factdoes exhibit some <strong>of</strong> the key features <strong>of</strong> the physical system it is intended todepict. It shows a phase transition at a critical temperature, and in general itsqualitative features show that we are mathematically on the right track, eventhough the numerical values we obtain from it are in fact not in accord withphysical measurements (Yeomans, 1992,Chapter4). In spite <strong>of</strong> the well-knownshortcomings <strong>of</strong> mean field theory, it is the usual starting point for workers instatistical mechanics investigating a new system (Fischer and Hertz, 1991,p.19).A partial explanation <strong>of</strong> the success <strong>of</strong> Weiss’s highly simplified model wasprovided by a Japanese physicist (Husimi, 1954), who pointed out that Weiss’smolecular field can be derived as the large N limit <strong>of</strong> a collection <strong>of</strong> classicalspin variables σ i =+1, −1, interacting through a Hamiltonian in which everyspin acts on every other spin—in the large N limit the interaction strengthis infinitesimal, that is to say, its strength is <strong>of</strong> order 1/N. The mathematicaldetails <strong>of</strong> Husimi’s observation were worked out later in (Kac, 1968)—see also(Thompson, 1972, §4.5).Physicists use the phrase ‘mean field model’ to refer to two distinct categories<strong>of</strong> model. The first is a model <strong>of</strong> the Weiss type, in which the collective action<strong>of</strong> a large set <strong>of</strong> microscopic variables is replaced by a macroscopic quantityrepresenting an average or mean; the second is an interaction model <strong>of</strong> thetype described by Husimi and Kac, in which microscopic variables (such asspins) interact with an unbounded number <strong>of</strong> other microsopic variables. Thetwo types <strong>of</strong> model, however, are not completely equivalent mathematically,even in the paradigmatic case <strong>of</strong> the Curie–Weiss model.It is clear in the case <strong>of</strong> mean field models that we are dealing withmathematical caricatures <strong>of</strong> physical systems, that nevertheless exhibit some <strong>of</strong>the most important broad features <strong>of</strong> critical phenomena and phase transitions.It is tempting to say that these models are simply mathematical objects in theirown right that are related in only a very rough and ready way to the real

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