A. Stephenson et Dk. Potter, TOWARDS A QUANTITATIVE DESCRIPTION OF FIELD-IMPRESSED ANISOTROPY OF SUSCEPTIBILITY, Geophysical journal international, 126(2), 1996, pp. 505-512
A simplified model of domain rearrangement in multidomain particles fo
llowing the application of an alternating (AF) or direct (DF) field is
used to quantify the dependence of anisotropy of magnetic susceptibil
ity on magnetic history. To be able to account for changes in the aver
age susceptibility (i.e. the average of three mutually perpendicular s
usceptibility measurements) of the sample following field treatment, t
he model has to be refined by introducing interaction between domains.
By fitting theoretical curves of anisotropy versus peak AF to experim
ental results for samples containing different size fractions of magne
tite particles, of average grain size ranging from 0.7 to 58 mu m, fou
r relevant parameters can be computed (for each sample), which enables
a good fit to be obtained. By allowing two of these parameters to cha
nge systematically when a DF is applied (and an IRM is acquired), the
anisotropy dependence on direct field strength can also be modelled. T
his includes the sign change observed as the field-impressed ellipsoid
changes from prolate to oblate, together with increases in the averag
e susceptibility as the field increases. However, some details, such a
s discrepancies between predicted and actual increases in the average
susceptibility at high fields, suggest that further refinement of the
model is required.