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arxiv: cond-mat/0412375 · v1 · submitted 2004-12-14 · ❄️ cond-mat.str-el · cond-mat.other

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The Role of Grain Boundaries in Determining the Transport Properties in Magnetite

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classification ❄️ cond-mat.str-el cond-mat.other
keywords boundariesgraincrystalmagnetiteroleaccompanyingaccountapparent
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We present magnetoresistance and Hall-effect measurements on single crystal magnetite Fe3O4 close to the Verwey transition Tv = 123.8 K. We show that the formation of grain boundaries accompanying the reduction in crystal symmetry plays a significant role in the electron scattering mechanism, and that grain boundaries can account for the apparent change in sign of the charge carriers below Tv.

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