Effects of Co2+ and Mn3+ ion substitutions on the anisotropy and magnetostriction constants of Y3Fe5O12

Abstract The results of room-temperature measurements of the magnetocrystalline anisotropy constants K 1 and K 2 are reported together with values of the magnetostriction constants λ 100 and λ 111 for single crystals of Y 3 Fe 5−2x Co x Si x O 12 , with x = 0, 0.007, and 0.028. As in the case of Co 2+ - Ge 4+ and Ru 4+ - Ca 2+ substitutions, K 1 becomes positive and K 2 more negative with increasing x. Significantly, λ 100 and λ 111 remain relatively unaffected by the presence of Co 2+ ions, in accord with the findings for Li 0.5 Fe 2.5 O 4 . Comparison is made with the Y 3 Fe 5−y Mn y O 12 system, and the ability to vary magnetostriction and anisotropy constants relatively independently by Mn 3+ or Co 2+ ion substitutions is explained.

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