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Philosophical Magazine | Vol.1, Issue.12 | | Pages 1147-1156

Philosophical Magazine

CXVI. Angles between partial magnetizations in spinel ferrites containing manganese ions of more than one valency

W. P. Osmond  
Abstract

In iron-deficient spinel ferrites containing manganese, but no other constituent of variable valency, all the manganese will not be divalent. Mn3+ ions tend to form strong directed semicovalent bonds in octahedral (B) sites but not in tetrahedral (A) sites. The reverse is true for Fe3+ ions. The antiparallel A[sbnd]B indirect exchange interaction should thus be weaker when one interacting ion is Mn3+ than when both are Fe3+. Any Mn3+ ions are likely to be coupled with parallel spins by double exchange with Mn2+ or Mn4+ ions in the same type of lattice site, The magnetic ions in either sublattice can then be considered as divided into two groups, one based on Mn3+ ions, and the other on Fe3+ ions, with different degrees of departure from antiparallelism of their net, spins to the net magnetization of the other sublattice. The molecular field approximation as applied by other authors to single ions is extended to such groups of ions, with certain provisos as to the correct interpretation to be given to the mathematical symbols used for interaction coefficients and angles between spin directions.

Original Text (This is the original text for your reference.)

CXVI. Angles between partial magnetizations in spinel ferrites containing manganese ions of more than one valency

In iron-deficient spinel ferrites containing manganese, but no other constituent of variable valency, all the manganese will not be divalent. Mn3+ ions tend to form strong directed semicovalent bonds in octahedral (B) sites but not in tetrahedral (A) sites. The reverse is true for Fe3+ ions. The antiparallel A[sbnd]B indirect exchange interaction should thus be weaker when one interacting ion is Mn3+ than when both are Fe3+. Any Mn3+ ions are likely to be coupled with parallel spins by double exchange with Mn2+ or Mn4+ ions in the same type of lattice site, The magnetic ions in either sublattice can then be considered as divided into two groups, one based on Mn3+ ions, and the other on Fe3+ ions, with different degrees of departure from antiparallelism of their net, spins to the net magnetization of the other sublattice. The molecular field approximation as applied by other authors to single ions is extended to such groups of ions, with certain provisos as to the correct interpretation to be given to the mathematical symbols used for interaction coefficients and angles between spin directions.

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W. P. Osmond,.CXVI. Angles between partial magnetizations in spinel ferrites containing manganese ions of more than one valency. 1 (12),1147-1156.

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