Hysteresis properties of magnetite and their dependence on particle size: A test of pseudo‐single‐domain remanence models
Author:
- David J. DunlopDDDavid J. Dunlop
- 10 August 1986
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 91 (B9) , 9569-9584
Abstract
This paper reports room temperature measurements of initial susceptibility χ0, second Rayleigh coefficient B, coercive force Hc, remanent coercive force HR, and the ratio Jrs/Js of near‐saturation remanent and induced magnetizations for four samples containing single‐crystal magnetite cubes with mean sizes of 0.037, 0.076, 0.10, and 0.22 μm. While χo and Hc have weak dependences on particle size d, Hc and Jrs vary strongly with size, as d−0.55 and d−0.75, respectively, over the 0.076–0.22 μm range. These hysteresis properties and their size dependences are incompatible with data for >l‐μm crushed and annealed magnetite grains. Nearly perfect unstrained crystals tend to have Hc and Jrs values 2–5 times smaller than those of pulverized grains of nominally the same size. Magnitudes and size dependences of Hc and Jrs for >0.06‐μm magnetites are approximately, although not perfectly, accounted for by (1) metastable single‐domain (SD) particles, (2) rotatable SD‐like domain wall (DW) moments, or (3) DW displacements impeded by crystal defects and limited by self‐demagnetization. Only reversible DW displacements (or possibly domain rotations) opposed by self−demagnetization can explain the initial susceptibility data, however.Keywords
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