MAGNETIC HYSTERESIS OF PSEUDO-SINGLE-DOMAIN AND MULTIDOMAIN MAGNETITE BELOW THE VERWEY TRANSITION

Show simple item record

dc.contributor.author Kosterov A.
dc.date.accessioned 2021-04-05T02:40:13Z
dc.date.available 2021-04-05T02:40:13Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=14002580
dc.identifier.citation Earth and Planetary Science Letters, 2001, 186, 2, 245-253
dc.identifier.issn 0012-821X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27294
dc.description.abstract Hysteresis loops have been measured as a function of temperature between 10 K and room temperature for two size fractions of crushed magnetite: 1–5 μm (pseudo-single-domain, PSD) and 100–150 μm (multidomain, MD). The material under study appears to be fairly close to stoichiometric magnetite, with a Verwey transition temperature of 115 K for the MD sample and 118 K for the PSD sample. For both samples, hysteresis properties below the Verwey transition depend critically on whether or not the samples were cooled through the transition in the magnetic field. For the PSD sample, an even more complex behavior has been observed: temperature dependences of coercive force obtained after zero-field-cooling differ significantly for the demagnetized versus magnetized starting magnetic state.
dc.title MAGNETIC HYSTERESIS OF PSEUDO-SINGLE-DOMAIN AND MULTIDOMAIN MAGNETITE BELOW THE VERWEY TRANSITION
dc.type Статья


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record