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Mossbauer Study of the Modulated Magnetic Structure of FeV[O.sub.4]

Mossbauer spectroscopy is used to study the FeV[O.sub.4] multiferroic, which undergoes two magnetic phase transitions at [T.sub.N1] ~ 22 K and [T.sub.N2] ~ 15 K. The first transition ([T.sub.N1]) is related to transformation from a paramagnetic state into a magnetically ordered state of a spin densi...

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Bibliographic Details
Published in:Journal of experimental and theoretical physics 2017-06, Vol.124 (6), p.943
Main Authors: Sobolev, A.V, Presnyakov, I.A, Rusakov, V.S, Gapochka, A.M, Glazkova, Ya.S, Matsnev, M.E, Pankratov, D.A
Format: Article
Language:English
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Summary:Mossbauer spectroscopy is used to study the FeV[O.sub.4] multiferroic, which undergoes two magnetic phase transitions at [T.sub.N1] ~ 22 K and [T.sub.N2] ~ 15 K. The first transition ([T.sub.N1]) is related to transformation from a paramagnetic state into a magnetically ordered state of a spin density wave, and the second transition ([T.sub.N2]) is associated with a change in the type of the spatial magnetic structure of the vanadate. The electric field gradient tensor at [sup.57]Fe nuclei is calculated to perform a crystal-chemical identification of the partial Mossbauer spectra corresponding to various crystallographic positions of [Fe.sup.3+] cations. The spectra measured in the range [T.sub.N2] < T < [T.sub.N1] are analyzed on the assumption about amplitude modulation of the magnetic moments of iron atoms [[mu].sub.Fe]. The results of model intersection of the spectra recorded at T < [T.sub.N2] point to a high degree of anharmonicity of the helicoidal magnetic structure of the vanadate and to elliptic polarization of [[mu].sub.Fe]. These features are characteristic of type-II multiferroics. The temperature dependences of the hyperfine interaction parameters of [sup.57]Fe nuclei that were obtained in this work are analyzed in terms of the Weiss molecular field model on the assumption of orbital contribution to the magnetic moments of iron cations.
ISSN:1063-7761
1090-6509
DOI:10.1134/S1063776117060164