Sensitivity of Curie Temperature to Crystal-Field Anisotropy. II. Fe
- 10 April 1967
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 156 (2) , 543-551
- https://doi.org/10.1103/physrev.156.543
Abstract
Fe is a simple two-sublattice antiferromagnet and has a rutile crystal structure. Its large anisotropy can be represented to a good approximation by single-ion crystal-field terms of the type discussed in Paper I. The purpose of the present paper is, firstly, to analyze relevant high- and low-temperature experimental data in order to estimate as accurately as possible the important exchange and anisotropy parameters for Fe and, secondly, to use this information to test the various theories for transition temperature which were the subject of Paper I. An adequate spin Hamiltonian for Fe can be written as where is over all pairs of nearest (next-nearest) neighbor spins and , and where is over all spins in the system. From an analysis of nuclear-resonance and magnetic-susceptibility data we find , , and . The resulting ratio takes Fe outside the small anisotropy range for which the theory of Paper I was primarily developed. Even so, use of the above parameter values in that theory results in a theoretical estimate for the Néel temperature which is in error by only some 12% for Fe. This estimate is considerably more accurate than those obtained by use of molecular-field theory or by earlier Green's-function approximations.
Keywords
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