High-resolution micromagnetic models of fine grains of magnetite

被引:40
作者
Williams, W
Wright, TM
机构
[1] Univ Edinburgh, Dept Geol & Geophys, Edinburgh EH9 3JW, Midlothian, Scotland
[2] Hewlett Packard Corp, Santa Rosa, CA USA
关键词
D O I
10.1029/98JB01120
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
High resolution three dimensional models are presented of cubic grains of magnetite in the grain size range 0.03 mu m to 4.0 mu m, achieved using a resolution of up to 262,144 elements to represent a single grain. Previous models have been limited in the maximum grain size that could be investigated because of the lack of resolution and increase in complexity of domain structure with grain size. This paper confirms the simple flower and vortex states found previously, but the classical two-domain (with closure domains) Kittel structure is shown not to be a local energy minimum state for magnetite. The concept of a single-domain to two-domain transition is now seen as a gradual unwinding of a flower state, and pseudo-single domain grains are shown to be vortex and multiple-vortex states. For grains greater than about 2 mu m in size the center of vortices act a nucleation centers for the formation of domain walls. At the largest grains size modeled (4.0 mu m), the expected features of multidomain grains are seen, with well-defined domain walls, and body domains with their magnetization aligned along the easy magnetocrystalline anisotropy axis.
引用
收藏
页码:30537 / 30550
页数:14
相关论文
共 35 条
[1]   Note on p-wave anomalies m proton-proton Scattering [J].
Breit, G ;
Kittel, C ;
Thaxton, HM .
PHYSICAL REVIEW, 1940, 57 (04) :255-259
[2]   THEORETICAL SINGLE-DOMAIN GRAIN-SIZE RANGE IN MAGNETITE AND TITANOMAGNETITE [J].
BUTLER, RF ;
BANERJEE, SK .
JOURNAL OF GEOPHYSICAL RESEARCH, 1975, 80 (29) :4049-4058
[3]   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
[4]   A MICROMAGNETIC STUDY OF PSEUDO SINGLE-DOMAIN REMANENCE IN MAGNETITE [J].
ENKIN, RJ ;
DUNLOP, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1987, 92 (B12) :12726-12740
[5]   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
[6]   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
[7]   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
[8]   Magnetic domain observations on magnetite and titanomaghemite grains (0.5-10 mu m) [J].
Geiss, CE ;
Heider, F ;
Soffel, HC .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1996, 124 (01) :75-88
[9]   THE DEPENDENCE OF MAGNETIC DOMAIN-STRUCTURE UPON MAGNETIZATION STATE WITH EMPHASIS UPON NUCLEATION AS A MECHANISM FOR PSEUDO-SINGLE-DOMAIN BEHAVIOR [J].
HALGEDAHL, S ;
FULLER, M .
JOURNAL OF GEOPHYSICAL RESEARCH, 1983, 88 (NB8) :6505-6522
[10]   MAGNETIC DOMAIN OBSERVATIONS OF NUCLEATION PROCESSES IN FINE PARTICLES OF INTERMEDIATE TITANOMAGNETITE [J].
HALGEDAHL, S ;
FULLER, M .
NATURE, 1980, 288 (5786) :70-72