THERMOMAGNETIC MEASUREMENTS OF SOIL IRON MINERALS: THE ROLE OF ORGANIC CARBON

Hanesch M.; Stanjek H.; Petersen N.

dc.contributor.author	Hanesch M.
dc.contributor.author	Stanjek H.
dc.contributor.author	Petersen N.
dc.date.accessioned	2024-12-07T09:08:18Z
dc.date.available	2024-12-07T09:08:18Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=14736950
dc.identifier.citation	Geophysical Journal International, 2006, 165, 1, 53-61
dc.identifier.issn	0956-540X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46915
dc.description.abstract	Thermomagnetic measurements, particularly measurements of the Curie or Néel temperature, are often used to identify magnetic minerals in rocks or sediments. In many samples it is impossible to determine the Curie or Néel temperature as mineral changes occur during heating. Especially in soils or sediments, iron (hydr)oxides may be transformed to ferrimagnetic iron oxides. In this study we analysed the thermomagnetic behaviour of some natural and synthetic iron minerals: goethite, haematite, ferrihydrite, lepidocrocite and siderite. The change of magnetization. © 2006 The Authors Journal compilation © 2006 RAS.
dc.subject	CURIE TEMPERATURE
dc.subject	IRON HYDROXIDES
dc.subject	NÉEL TEMPERATURE
dc.subject	SOIL MAGNETISM
dc.title	THERMOMAGNETIC MEASUREMENTS OF SOIL IRON MINERALS: THE ROLE OF ORGANIC CARBON
dc.type	Статья
dc.identifier.doi	10.1111/j.1365-246X.2006.02933.x