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dc.contributor.author Stull, John Leete
dc.date.accessioned 2014-02-27T21:11:29Z
dc.date.available 2014-02-27T21:11:29Z
dc.date.issued 1954-02-01
dc.identifier.uri http://hdl.handle.net/10829/5584
dc.description.abstract The 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.sponsorship Office of Naval Research en_US
dc.language.iso en-US en_US
dc.publisher Alfred University. Faculty of Ceramic Engineering. Kazuo Inamori School of Engineering en_US
dc.subject Stull, John en_US
dc.subject Magnetostriction en_US
dc.subject Magnetite en_US
dc.title Magnetostriction of Magnetite en_US
dc.type Thesis en_US


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