1998
DOI: 10.1071/p97066
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A Review of the Low Temperature Properties of the Rare Earth Vanadates

Abstract: The rare earth vanadates have long been studied for their interesting magnetic properties and cooperative Jahn–Teller distortions. In the main, most of this work has been carried out at temperatures down to 1 K or so (e.g. Gehring and Gehring 1975). In this review NMRON, and other low temperature experiments in the mK regime, are presented and discussed. It will be argued that the low temperature properties of these compounds are just as interesting as their high temperature counterparts. In general, the nucle… Show more

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Cited by 30 publications
(35 citation statements)
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References 47 publications
(73 reference statements)
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“…Such doublet can be described by an effective spin S= 1 2 and a spectroscopic g-tensor which, in the case of axial symmetry, has two components g z and g > defined by 4 : g z ¼ 6:08 and g > =0.85 [4]. Surprisingly, in the magnetically ordered state, the Yb moments do not lie along the easy c-axis but in the a-b plane, which constitutes a hard magnetic plane.…”
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confidence: 99%
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“…Such doublet can be described by an effective spin S= 1 2 and a spectroscopic g-tensor which, in the case of axial symmetry, has two components g z and g > defined by 4 : g z ¼ 6:08 and g > =0.85 [4]. Surprisingly, in the magnetically ordered state, the Yb moments do not lie along the easy c-axis but in the a-b plane, which constitutes a hard magnetic plane.…”
mentioning
confidence: 99%
“…For a polycrystalline sample, the saturated magnetisation of an extremely anisotropic doublet (i.e. g > /g z 51) averaged over all orientations is ence in the magnetic ordering temperature between the isostructural YbCrO 4 (T C =25 K) and YbVO 4 (T N =93 mK) oxides, coupled with a different sign of the magnetic interactions and the alignment of the Yb 3+ magnetic moments along the a-b plane in the YbCrO 4 oxide, points to the dominant role that the Cr 5+ magnetic ion plays in determining the overall magnetic ordering temperature, as well as polarising the magnetic moments of the Yb 3+ ions along a hard direction of magnetisation.…”
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“…They crystallize into two different structural types: monazite (monoclinic symmetry, S. G. P2 1 /c) or zircon (tetragonal symmetry, S. G. I4 1 /amd), depending on the size of both the R(III) and the X(V) ions [1][2][3]. They have been subject to extensive studies concerning their optical and magnetic properties [4,5]. Rare earth chromates present two magnetic ions in the lattice, namely R(III) and Cr(V), so that they constitute an ideal tool to asses the nature of the magnetic 3d-4f interactions.…”
Section: Introductionmentioning
confidence: 99%