The idea of forming invariants from the critical amplitudes of ferromagnets is extended to include the specific-heat amplitudes. Hence for planar Ising lattices it is shown that current estimates of the bulk susceptibility amplitudes are of great consistency, and that surface properties all become isotropic in the critical region. A hypothesis of Fisk and Widom about the equation of state is confirmed.
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Peter Watson (1969) studied this question.
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