EFFECT OF THE PRESSURE AND THE RARE-EARTH SUBSTITUTION ON THE VERWEY TRANSITION OF YFE2O4

被引:11
作者
SIRATORI, K
MORI, N
TAKAHASHI, H
OOMI, G
IIDA, J
TANAKA, M
KISHI, M
NAKAGAWA, Y
KIMIZUKA, N
机构
[1] HOKKAIDO UNIV,FAC SCI,SAPPORO,HOKKAIDO 060,JAPAN
[2] UNIV TOKYO,INST SOLID STATE PHYS,MINATO KU,TOKYO 113,JAPAN
[3] OCHANOMIZU UNIV,FAC SCI,BUNKYO KU,TOKYO 112,JAPAN
[4] TOHOKU UNIV,INST MAT RES,SENDAI,MIYAGI 980,JAPAN
[5] NAT INST RES INORGAN MAT,TSUKUBA,IBARAKI,JAPAN
关键词
D O I
10.1143/JPSJ.59.631
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Effects of the hydrostatic pressure as well as the rare earth substitution are examined on the two-step Verwey transition of the stoichiometric YFe2O4, by the electric and the magnetic measurements. The upper and the lower transition temperatures decrease with the compression by 2.6 and 10.5 K/kb, respectively. Substitution of Y by Lu decreases whereas that by Dy increases the transition temperature. At room temperature in the high conductivity phase, lattice constants in the hexagonal frame, a and c, are measured for substituted crystals and for the stoichiometric YFe2O4 under pressure. It is shown that the upper and the lower transition temperatures are independent from c but decrease 10 and 42 K, respectively, by 10-3 compression of the lattice along the a axis. The character of the transition is discussed briefly. © 1990, THE PHYSICAL SOCIETY OF JAPAN. All rights reserved.
引用
收藏
页码:631 / 636
页数:6
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