Changes in remanence, coercivity and domain state at low temperature in magnetite

被引:152
作者
Özdemir, Ö [1 ]
Dunlop, DJ
Moskowitz, BM
机构
[1] Univ Toronto, Dept Phys, Mississauga, ON L5L 1C6, Canada
[2] Univ Minnesota, Inst Rock Magnetism, Minneapolis, MN 55455 USA
基金
加拿大自然科学与工程研究理事会; 美国国家科学基金会;
关键词
magnetite; hysteresis; magnetic domains; coercivity; remanent magnetization;
D O I
10.1016/S0012-821X(01)00562-3
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Submicron magnetite crystals with mean sizes of 0.037, 0.10 and 0.22 mum undergo major changes in hysteresis properties and domain states in crossing the Verwey transition (T-v approximate to 120 K). The 0,037 mum crystals are single-domain (SD) both in the cubic phase at room temperature T-0 and in the monoclinic phase below T-v. The 0.10 and 0.22 mum crystals have a mixture of SD and two-domain (2D) states at room temperature T-0 but mainly SD structures below T-v, in agreement with micromagnetic calculations. Coercive force H-c increases on cooling through T-v, by a factor 3-5 in the submicron magnetites and 40 in a 1.3 mm, single crystal, because of the high crystalline anisotropy and magnetostriction of monoclinic magnetite. As a result, domain walls and SD moments are so effectively pinned below T-v that all remanence variations in warming or cooling are reversible. However, between approximate to 100 K and T-0, remanence behavior is variable. Saturation remanence (SIRM) produced in monoclinic magnetite at 5 K drops by 70-100% in warming across T-v, with minor recovery in cooling back through T-v (ultimate levels at 5 K of 23-37% for the submicron crystals and 3% for the 1.3 mm crystal). In contrast, SIRM produced in the cubic phase at 300 K decreases 5-35% (submicron) or > 95% (1.3 mm) during cooling from 300 to 120 K due to continuous re-equilibration of domain walls, but there is little further change in cooling through T-v itself. However, the submicron magnetites lose a further 5-15% of their remanence when reheated through T-v. These irreversible changes in cycling across T-v, and the amounts of the changes, have potential value in determining submicron magnetite grain sizes. The irreversibility is mainly caused by 2D-->SD transformations on cooling through T-v, which preserve or enhance remanence, while SD-->2D transformations on warming through T-v cause remanence to demagnetize. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:343 / 358
页数:16
相关论文
共 44 条
[1]   MAGNETOCRYSTALLINE ANISOTROPY OF LOW-TEMPERATURE PHASE OF MAGNETITE [J].
ABE, K ;
MIYAMOTO, Y ;
CHIKAZUMI, S .
JOURNAL OF THE PHYSICAL SOCIETY OF JAPAN, 1976, 41 (06) :1894-1902
[2]  
Chikazumi S., 1971, FERRITES, P141
[3]   HYSTERESIS PROPERTIES OF TITANOMAGNETITES - GRAIN-SIZE AND COMPOSITIONAL DEPENDENCE [J].
DAY, R ;
FULLER, M ;
SCHMIDT, VA .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1977, 13 (04) :260-267
[4]   SUPERPARAMAGNETIC AND SINGLE-DOMAIN THRESHOLD SIZES IN MAGNETITE [J].
DUNLOP, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (11) :1780-1793
[5]   HYSTERESIS PROPERTIES OF MAGNETITE AND THEIR DEPENDENCE ON PARTICLE-SIZE - A TEST OF PSEUDO-SINGLE-DOMAIN REMANENCE MODELS [J].
DUNLOP, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1986, 91 (B9) :9569-9584
[6]   Paleomagnetism and paleothermometry of the Sydney Basin .1. Thermoviscous and chemical overprinting of the Milton Monzonite [J].
Dunlop, DJ ;
Schmidt, PW ;
Ozdemir, O ;
Clark, DA .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1997, 102 (B12) :27271-27283
[7]   MAGNETITE - BEHAVIOR NEAR SINGLE-DOMAIN THRESHOLD [J].
DUNLOP, DJ .
SCIENCE, 1972, 176 (4030) :41-&
[9]   HUNTING OF PSARK [J].
DUNLOP, DJ .
JOURNAL OF GEOMAGNETISM AND GEOELECTRICITY, 1977, 29 (04) :293-318
[10]  
DUNLOP DJ, 2001, IN PRESS J GEOPHYS R, V106