First-order reversal curve (FORC) diagrams for pseudo-single-domain magnetites at high temperature
File(s)muxworthy-dunlop-2002.pdf (1.92 MB)
Accepted version
Author(s)
Muxworthy, AR
Dunlop, DJ
Type
Journal Article
Abstract
The recently developed first-order reversal curve (FORC) technique for rapidly examining magnetic domain state has great potential for paleomagnetic and environmental magnetic investigations. However, there are still some gaps in the basic understanding of FORC diagrams, in particular the behavior of pseudo-single-domain (PSD) grains and the contribution of magnetostatic interactions. In this paper we address some of these problems. We report the first FORC diagrams measurements on narrowly sized and well-characterized synthetic PSD through multidomain (MD) magnetite samples. The FORC diagrams evolve with grain size from single-domain (SD)-like to MD-like through the PSD grain size range. Since each sample contains grains of essentially a single size, individual PSD grains evidently contain contributions from both SD-like and MD-like magnetic moments, in proportions that vary with grain size; the evolving FORC diagrams cannot be due to physical mixtures of SD and MD grains of widely different sizes. The FORC diagrams were all asymmetric. Small PSD samples have FORC diagrams with a distinctive closed-contour structure. The distributions of the larger MD grains display no peak, and lie closer to the interaction-field axis. To assess the effect of magnetostatic interactions, we measured FORC diagrams between room temperature and the Curie temperature. On heating the FORC distributions contract without changing shape until similar to500degreesC. Above this temperature the diagrams become more MD-like, and in addition become more symmetric. The temperature dependence of the interaction-field parameter is proportional to that of the saturation magnetization, in accordance with Neel's interpretation of the Preisach diagram. The decrease in asymmetry with heating suggests that the origin of the asymmetry lies in magnetostatic interactions. The magnetic hysteresis parameters as a function of temperature were determined from the FORC curves. As the grain size decreased the normalized coercive force was found to decrease more rapidly with temperature. (C) 2002 Elsevier Science B.V. All rights reserved.
Version
Accepted version
Date Issued
2002-10-15
Citation
EARTH PLANET SC LETT, 2002, 203 (1), pp.369-382
ISSN
0012-821X
Publisher
ELSEVIER SCIENCE BV
Start Page
369
End Page
382
Journal / Book Title
EARTH PLANET SC LETT
Volume
203
Issue
1
Copyright Statement
© 2002 Elsevier Science B.V. This is the author’s version of a work that was accepted for publication in Earth and Planetary Science Letters. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Earth and Planetary Science Letters, volume 203, issue 1 (October 2002). doi:
10.1016/S0012-821X(02)00880-4
10.1016/S0012-821X(02)00880-4
Source Volume Number
203
Subjects
magnetite
magnetic domains
coercivity
reversals
CRYSTAL DEFECTS
HYSTERESIS
SAMPLES
DEPENDENCE
MODELS
Coverage Spatial
Nice, France