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Detailed Reference Information |
Menyeh, A. and O'Reilly, W. (1998). Thermoremanence in monoclinic pyrrhotite particles containing few domains. Geophysical Research Letters 25: doi: 10.1029/98GL02220. issn: 0094-8276. |
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The intensity and stability of thermoremanent magnetization (TRM) acquired by synthetic Fe7S8 particles in the size range 1--29 &mgr;m has been determined. The intensity falls with increasing particle size. The unblocking temperature increases with increasing particle size. The intensity-particle size dependence can be fitted to a theory, in which a fraction of the particles fails to nucleate a domain wall on cooling, only if the TRM of the resultant monodomain fraction is much smaller than that expected of crystals of this size. This could arise if the particles were made of nanocrystals of much smaller size. The data may be given a much simpler theoretical description by adopting a particle size dependent effective demagnetizing factor with a fully formed domain structure with highly mobile walls above the blocking temperature. ¿ 1998 American Geophysical Union |
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Abstract |
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Keywords
Physical Properties of Rocks, Magnetic and electrical properties, Physical Properties of Rocks, Thermal properties |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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