Rare earth contribution to the hyperfine field acting on 119Sn in rare earth iron garnets

E. R. Bauminger; J. Hess; I. Nowik; S. Ofer

doi:10.1016/0038-1098(72)90443-7

Rare earth contribution to the hyperfine field acting on ¹¹⁹Sn in rare earth iron garnets

E. R. Bauminger^*, J. Hess, I. Nowik, S. Ofer

^*Corresponding author for this work

Racah Institute of Physics

Research output: Contribution to journal › Article › peer-review

4 Scopus citations

Abstract

The rare earth contribution (-27 ± 2 koe in GdIG) to the hyperfine field acting on ¹¹⁹Sn in iron garnets has been found to be a monotonic, but not a linear function of the experimental value of the rare earth ionic spin. This non-linearity is due to an anisotropic transfer mechanism. The ratio of g_ex/g_o in ¹¹⁹Sn was found to be -0.2154 ± 0.0002.

Original language	English
Pages (from-to)	365-367
Number of pages	3
Journal	Solid State Communications
Volume	10
Issue number	4
DOIs	https://doi.org/10.1016/0038-1098(72)90443-7
State	Published - 15 Feb 1972

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title = "Rare earth contribution to the hyperfine field acting on 119Sn in rare earth iron garnets",

abstract = "The rare earth contribution (-27 ± 2 koe in GdIG) to the hyperfine field acting on 119Sn in iron garnets has been found to be a monotonic, but not a linear function of the experimental value of the rare earth ionic spin. This non-linearity is due to an anisotropic transfer mechanism. The ratio of gex/go in 119Sn was found to be -0.2154 ± 0.0002.",

author = "Bauminger, {E. R.} and J. Hess and I. Nowik and S. Ofer",

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AU - Nowik, I.

AU - Ofer, S.

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Y1 - 1972/2/15

N2 - The rare earth contribution (-27 ± 2 koe in GdIG) to the hyperfine field acting on 119Sn in iron garnets has been found to be a monotonic, but not a linear function of the experimental value of the rare earth ionic spin. This non-linearity is due to an anisotropic transfer mechanism. The ratio of gex/go in 119Sn was found to be -0.2154 ± 0.0002.

AB - The rare earth contribution (-27 ± 2 koe in GdIG) to the hyperfine field acting on 119Sn in iron garnets has been found to be a monotonic, but not a linear function of the experimental value of the rare earth ionic spin. This non-linearity is due to an anisotropic transfer mechanism. The ratio of gex/go in 119Sn was found to be -0.2154 ± 0.0002.

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Rare earth contribution to the hyperfine field acting on ¹¹⁹Sn in rare earth iron garnets

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