Magnetostriction of Magnetite

dc.contributor.authorStull, John Leete
dc.date.accessioned2014-02-27T21:11:29Z
dc.date.available2014-02-27T21:11:29Z
dc.date.issued1954-02-01
dc.description.abstractThe magnetostriction of Fe3O4 was measured, using the strain gauge technique. Two methods were used to measure the magnetostrictive behavior of single crystals and polycrystalline samples as a function of orientation and temperature. The measurements show that magnetostriction does not play an important part in causing a peak in initial permeability in magnetite near its low-temperature transition. Another conclusion is that magnetostriction measurements can be used for this type of material as a tool to detect changes in the direction of easy magnetization.en_US
dc.description.sponsorshipOffice of Naval Researchen_US
dc.identifier.urihttp://hdl.handle.net/10829/5584
dc.language.isoen-USen_US
dc.publisherAlfred University. Faculty of Ceramic Engineering. Kazuo Inamori School of Engineeringen_US
dc.subjectStull, Johnen_US
dc.subjectMagnetostrictionen_US
dc.subjectMagnetiteen_US
dc.titleMagnetostriction of Magnetiteen_US
dc.typeThesisen_US

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