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dc.contributor.authorYang, X.
dc.contributor.authorAldrich, Chris
dc.date.accessioned2017-01-30T11:18:01Z
dc.date.available2017-01-30T11:18:01Z
dc.date.created2015-03-03T03:51:01Z
dc.date.issued2008
dc.identifier.citationYang, X. and Aldrich, C. 2008. Sedimentation of Magnetic Suspensions of Magnetite. The Open Mineral Processing Journal. 1: pp. 18-25.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/10319
dc.description.abstract

The gravity sedimentation of three narrow-sized fractions of suspensions of magnetite particles exposed to magnetic fields ranging from 0 to 180 x 10-4 T was studied experimentally. At volumetric solids concentrations in excess of 15%, the magnetized suspensions of magnetite with size fractions ranging from -75 to +38 µm settled more slowly than the non-magnetized suspensions. However, owing to relatively weak magnetic interaction, the sedimentation of the magnetized and non-magnetized -38 µm size fractions was similar.

dc.publisherBentham Science
dc.titleSedimentation of Magnetic Suspensions of Magnetite
dc.typeJournal Article
dcterms.source.volume1
dcterms.source.startPage18
dcterms.source.endPage25
dcterms.source.issn1874-8414
dcterms.source.titleThe Open Mineral Processing Journal
curtin.accessStatusFulltext not available


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