Abstract
The demagnetization constant', N, enters into all theoretical considerations of multidomain remanence. Although most workers believe N to be related simply to the shape of the grain, no theoretical study of N has previously been completed. It is shown in this paper that N monotonically increases with increase in remanence in multidomain grains. Although N can be approximated by a constant in the limit of small displacements of domain walls from their demagnetized sites, this constant critically depends on the domain geometry. © 1977, Society of Geomagnetism and Earth, Planetary and Space Sciences. All rights reserved.
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CITATION STYLE
Merrill, R. T. (1977). The Demagnetization Field of Multidomain Grains. Journal of Geomagnetism and Geoelectricity, 29(4), 285–292. https://doi.org/10.5636/jgg.29.285
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