Abstract
It was shown by measurements in static magnetic fields that, contrary to the results obtained byMcKinnon et al. in pulsedf elds, the critical field for the antiferromagnetic-ferromagnetic (AFM-FM) transition in FeRh is a nearly linear function of temperature. The linear temperature dependence suggests that besides the electronic contribution there must be a considerable lattice contribution to the entropy change observed in the AFM-FM transition.
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