Large (H,D) isotope effect on the metamagnetic transition in Y0.9R0.1Fe2(H,D)4.3
 compounds

Leblond, T.; Paul-Boncour, V.; Guillot, M.

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Large (H,D) isotope effect on the metamagnetic transition in Y_0.9R_0.1Fe₂(H,D)_4.3 compounds

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Guillot, M.
High Magnetic Field Laboratory, Former Departments, Max Planck Institute for Solid State Research, Max Planck Society;

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Citation

Leblond, T., Paul-Boncour, V., & Guillot, M. (2006). Large (H,D) isotope effect on the metamagnetic transition in Y_0.9R_0.1Fe₂(H,D)_4.3 compounds. Journal of Applied Physics, 99(8): 08F505.

Cite as: https://hdl.handle.net/21.11116/0000-000E-FB3D-4

Abstract

The influence of the (H,D) isotope substitution on the metamagnetic
transition in (Y1-xRx)Fe-2(H1-yDy)(4.2) (R=Tb, Er, x=0, 0.1, and y=0,
1) compounds has been studied by x-ray diffraction and magnetic
measurements. All these compounds crystallize in the same monoclinic
structure with larger cell volume for the hydrides compared to the
deuterides. The metamagnetic transition temperature T-M is not only
field dependent but also strongly related to the volume change. The
increase of T-M is more strongly related to the (H,D) isotope
substitution than by the rare earth substitution on the Y site. (C)
2006 American Institute of Physics.