High-temperature magnetic stability of small magnetite particles

被引:43
作者
Muxworthy, AR
Dunlop, DJ
Williams, W
机构
[1] Univ Edinburgh, Sch Geosci, Grant Inst, Edinburgh EH9 3JW, Midlothian, Scotland
[2] Univ Toronto, Dept Phys, Toronto, ON, Canada
关键词
micromagnetism; transdomain; thermoremanent magnetisation; magnetic stability; magnetic structures; magnetite;
D O I
10.1029/2002JB002195
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
The stability of magnetic domain structures of small grains of magnetite were examined between room temperature and the Curie temperature using a high-resolution three-dimensional micromagnetic algorithm. At all times the minimum resolution used was determined by calculating the exchange length. Using an unconstrained model, the single domain (SD) to multidomain (MD) threshold grain size d(0) was found to be nearly independent of temperature up to similar to450degreesC. Above this temperature, d(0) was observed to rise sharply. Energy barriers between metastable domain states trapped in local energy minimums (LEM) were determined using a constrained algorithm. Three types of domain structure were considered: SD, vortex, and double vortex (effectively three domain), in a range of grain sizes with side length between 30 and 300 nm. In addition, the effect of varying shape was also considered by examining asymmetric grains with aspect ratios up to 1.4. From the numerical solutions energy barriers between LEM states were determined. It was found that MD grains 300 nm in size display higher stability than smaller SD grains (similar to50 nm). Double vortex states were found to be less stable than single vortex states at nearly all temperatures. Blocking temperatures as function of grain size for both symmetric and asymmetric grains were determined and agree well with experimental results. Transdomain thermoremanence analysis indicated that there are a limited number of grain sizes and shapes which will nucleate domain wall-type structures during cooling. Such nucleation events would cause the total measured remanence to decrease with cooling in conflict with Neel's analytical theory for remanence cooling behavior but in agreement with experimental observations.
引用
收藏
页数:9
相关论文
共 30 条
[1]   THERMOREMANENT MAGNETIZATION IN SUBMICROSCOPIC MAGNETITE [J].
DUNLOP, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (32) :7602-7613
[2]   SEPARATING MULTIDOMAIN AND SINGLE-DOMAIN-LIKE REMANENCES IN PSEUDO-SINGLE-DOMAIN MAGNETITES (215-540 NM) BY LOW-TEMPERATURE DEMAGNETIZATION [J].
DUNLOP, DJ ;
ARGYLE, KS .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1991, 96 (B2) :2007-2017
[3]   TRANSDOMAIN THERMOREMANENT MAGNETIZATION [J].
DUNLOP, DJ ;
NEWELL, AJ ;
ENKIN, RJ .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1994, 99 (B10) :19741-19755
[5]   AN EXPERIMENTAL EVALUATION OF SINGLE DOMAIN THEORIES [J].
DUNLOP, DJ ;
WEST, GF .
REVIEWS OF GEOPHYSICS, 1969, 7 (04) :709-&
[6]   3-DIMENSIONAL MICROMAGNETIC ANALYSIS OF STABILITY IN FINE MAGNETIC GRAINS [J].
ENKIN, RJ ;
WILLIAMS, W .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1994, 99 (B1) :611-618
[7]   Three-dimensional micromagnetic calculations for magnetite using FFT [J].
Fabian, K ;
Kirchner, A ;
Williams, W ;
Heider, F ;
Leibl, T ;
Hubert, A .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1996, 124 (01) :89-104
[8]   How to include magnetostriction in micromagnetic models of titanomagnetite grains [J].
Fabian, K ;
Heider, F .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (20) :2839-2842
[9]   CONTRIBUTION OF FE2+ IONS TO MAGNETOCRYSTALLINE ANISOTROPY CONSTANT K1 OF FE3-XTIXO4(O LESS THAN X LESS THAN 0.1) [J].
FLETCHER, EJ ;
OREILLY, W .
JOURNAL OF PHYSICS C-SOLID STATE PHYSICS, 1974, 7 (01) :171-178
[10]   NOTE ON TEMPERATURE-DEPENDENCE OF EXCHANGE CONSTANT IN MAGNETITE [J].
HEIDER, F ;
WILLIAMS, W .
GEOPHYSICAL RESEARCH LETTERS, 1988, 15 (02) :184-187