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Magnetic force microscopy of single crystal magnetite (Fe3O4)(abstract)

dc.contributor.authorProksch, R.en_US
dc.contributor.authorFoss, S.en_US
dc.contributor.authorOrme, C.en_US
dc.contributor.authorSahu, S.en_US
dc.contributor.authorMoskowitz, B.en_US
dc.date.accessioned2010-05-06T21:47:59Z
dc.date.available2010-05-06T21:47:59Z
dc.date.issued1994-05-15en_US
dc.identifier.citationProksch, R.; Foss, S.; Orme, C.; Sahu, S.; Moskowitz, B. (1994). "Magnetic force microscopy of single crystal magnetite (Fe3O4)(abstract)." Journal of Applied Physics 75(10): 6892-6892. <http://hdl.handle.net/2027.42/70207>en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/70207
dc.description.abstractThe micromagnetic domain structure of a magnetite (Fe3O4) single crystal has been studied using a magnetic force microscope (MFM). The MFM responds to the perpendicular component of the stray field above the magnetite surface. The sample was polished in the (011) plane. In this case, there are two easy magnetic axes parallel to the surface. Surface domains observed near cracks and edges have a complex closure structure (see Fig. 1), while walls seen far from such boundaries have a sinusoidal structure. Of particular interest is the presence of walls with either even or odd symmetry of the perpendicular stray field component across the transition. These can be conventionally modeled as Bloch or Neel walls, respectively. Both types of walls have been modeled and compared with the experimentally observed structures. We find the Bloch domain walls to be about 300 nm wide, nearly twice the value expected from bulk wall calculations. This distinction is consistent with a surface broadening of the domain wall due to magnetostatic effects.en_US
dc.format.extent3102 bytes
dc.format.extent66541 bytes
dc.format.mimetypetext/plain
dc.format.mimetypeapplication/pdf
dc.publisherThe American Institute of Physicsen_US
dc.rights© The American Institute of Physicsen_US
dc.titleMagnetic force microscopy of single crystal magnetite (Fe3O4)(abstract)en_US
dc.typeArticleen_US
dc.subject.hlbsecondlevelPhysicsen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Physics, University of Michigan, Ann Arbor, Michiganen_US
dc.contributor.affiliationotherSchool of Physics and Astronomy, University of Minnesota, Minneapolis, Minnesota 55455en_US
dc.contributor.affiliationotherInstitute for Rock Magnetism, University of Minnesota, Minneapolis, Minnesota 55455en_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/70207/2/JAPIAU-75-10-6892-1.pdf
dc.identifier.doi10.1063/1.356771en_US
dc.identifier.sourceJournal of Applied Physicsen_US
dc.identifier.citedreferenceM. R. Scheinfein, J. Unguris, R. J. Celotta, and D. T. Pierce, Phys. Rev. Lett. 63, 668 (1989).en_US
dc.owningcollnamePhysics, Department of


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