Magnetic field-induced phase transition in ilmenite-type CoVO3

Author:

Yamamoto Hajime1ORCID,Wu Hung-Cheng1ORCID,Miyake Atsushi2ORCID,Tokunaga Masashi2ORCID,Suzuki Akio3ORCID,Honda Takashi4ORCID,Kimura Hiroyuki1

Affiliation:

1. Institute of Multidisciplinary Research for Advanced Materials, Tohoku University 1 , Katahira 2-1-1, Aoba-ku, Sendai 980-8577, Japan

2. Institute for Solid State Physics, University of Tokyo 2 , Kashiwanoha 5-1-5, Kashiwa, Chiba 277-8581, Japan

3. Department of Earth Science, Graduate School of Science, Tohoku University 3 , 6-3, Aramaki Aza-Aoba, Aoba-ku, Sendai 980-8578, Japan

4. Institute of Materials Structure Science, High Energy Accelerator Research Organization (KEK) 4 , Oho 1-1, Tsukuba, Ibaraki 305-0801, Japan

Abstract

The ilmenite-type CoVO3 undergoes an antiferromagnetic transition below 140 K, and the tetravalent vanadium ions form V–V dimers below 550 K. This paper presents the magnetic spin structure and the phase transition induced by a magnetic field in CoVO3. Neutron powder diffraction at 50 K reveals that the spins of Co2+ arrange in a zigzag order on the honeycomb lattice with no external magnetic field. This magnetic spin structure does not exhibit spontaneous magnetization, corroborating previous magnetic measurements. Magnetization measurements in a pulsed-magnetic field revealed a transition to a weak-ferromagnetic phase at 37 T (100 K) and above 50 T (4.2 K), with spontaneous magnetization approximating 0.3–0.5 μB/f.u. This phase transition could potentially be attributed to a transition to a canted antiferromagnetic phase, which is brought about by the reduction in structural symmetry due to magnetostriction.

Publisher

AIP Publishing

Subject

Physics and Astronomy (miscellaneous)

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