Two separate theories are often used to characterize the paramagnetic properties of ferromagnetic materials. At temperatures T well above the Curie temperature, T(C) (where the transition from paramagnetic to ferromagnetic behaviour occurs), classical mean-field theory yields the Curie-Weiss law for the magnetic susceptibility: χ(T) proportional to 1/(T - Θ), where Θ is the Weiss constant. Close to T(C), however, the standard mean-field approach breaks down so that better agreement with experimental data is provided by critical scaling theory: χ(T) proportional to 1/(T - T(C))(γ) where γ is a scaling exponent. But there is no known model capable of predicting the measured values of γ nor its variation among different substances. Here I use a mean-field cluster model based on finite-size thermostatistics to extend the range of mean-field theory, thereby eliminating the need for a separate scaling regime. The mean-field approximation is justified by using a kinetic-energy term to maintain the microcanonical ensemble. The model reproduces the Curie-Weiss law at high temperatures, but the classical Weiss transition at T(C) = Θ is suppressed by finite-size effects. Instead, the fraction of clusters with a specific amount of order diverges at T(C), yielding a transition that is mathematically similar to Bose-Einstein condensation. At all temperatures above T(C) the model matches the measured magnetic susceptibilities of crystalline EuO, Gd, Co and Ni, thus providing a unified picture for both the critical-scaling and Curie-Weiss regimes.
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