FIRST-ORDER REVERSAL CURVE (FORC) DIAGRAMS FOR PSEUDO-SINGLE-DOMAIN MAGNETITES AT HIGH TEMPERATURE

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dc.contributor.author Muxworthy A.R.
dc.contributor.author Dunlop D.J.
dc.date.accessioned 2021-09-17T06:49:06Z
dc.date.available 2021-09-17T06:49:06Z
dc.date.issued 2002
dc.identifier https://elibrary.ru/item.asp?id=1251787
dc.identifier.citation Earth and Planetary Science Letters, 2002, 203, 1, 369-382
dc.identifier.issn 0012-821X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/30282
dc.description.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 ~500°C. 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.
dc.subject MAGNETITE
dc.subject MAGNETIC DOMAINS
dc.subject COERCIVITY
dc.subject REVERSALS
dc.title FIRST-ORDER REVERSAL CURVE (FORC) DIAGRAMS FOR PSEUDO-SINGLE-DOMAIN MAGNETITES AT HIGH TEMPERATURE
dc.type Статья


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