Thermodynamics of Fe(II)Fe(III) oxide systems I. Hydrothermal Fe3O4
dc.contributor.author | Bartel, James J. | en_US |
dc.contributor.author | Westrum, Jr. , Edgar F. | en_US |
dc.contributor.author | Haas, Jr. , John L. | en_US |
dc.date.accessioned | 2006-04-07T16:33:09Z | |
dc.date.available | 2006-04-07T16:33:09Z | |
dc.date.issued | 1976-06 | en_US |
dc.identifier.citation | Bartel, James J., Westrum, Jr., Edgar F., Haas, Jr., John L. (1976/06)."Thermodynamics of Fe(II)Fe(III) oxide systems I. Hydrothermal Fe3O4." The Journal of Chemical Thermodynamics 8(6): 575-581. <http://hdl.handle.net/2027.42/21916> | en_US |
dc.identifier.uri | http://www.sciencedirect.com/science/article/B6WHM-4CRH94D-DT/2/e1170b8593807c318f181cbd3d095f20 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/21916 | |
dc.description.abstract | The heat capacity of a hydrothermally-prepared polycrystalline sample of Fe3O4 was measured from 53 to 350 K, primarily to study the thermophysics of the Verwey transitions. Although the bifurcation of the transition was confirmed, the sample was found to contain traces of manganese. The observed transition temperatures of 117.0 and 123.0 K are 3.7 and 4.2 K higher respectively than those found in pure Fe3O4. Ancillary analytical results are consistent and indicate a stoichiometry of Mn0.008Fe2.992O4 for this material. Characteristics in the transition region are ascribed to dopant effects. | en_US |
dc.format.extent | 404863 bytes | |
dc.format.extent | 3118 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Elsevier | en_US |
dc.title | Thermodynamics of Fe(II)Fe(III) oxide systems I. Hydrothermal Fe3O4 | en_US |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | en_US |
dc.subject.hlbsecondlevel | Materials Science and Engineering | en_US |
dc.subject.hlbsecondlevel | Chemistry | en_US |
dc.subject.hlbsecondlevel | Chemical Engineering | en_US |
dc.subject.hlbsecondlevel | Biological Chemistry | en_US |
dc.subject.hlbtoplevel | Engineering | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.subject.hlbtoplevel | Health Sciences | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Chemistry, University of Michigan, Ann Arbor, Michigan 48104, U.S.A.; U.S. Geological Survey, National Center, Stop 959, Reston, Virginia 22092, U.S.A. | en_US |
dc.contributor.affiliationum | Department of Chemistry, University of Michigan, Ann Arbor, Michigan 48104, U.S.A.; U.S. Geological Survey, National Center, Stop 959, Reston, Virginia 22092, U.S.A. | en_US |
dc.contributor.affiliationum | Department of Chemistry, University of Michigan, Ann Arbor, Michigan 48104, U.S.A.; U.S. Geological Survey, National Center, Stop 959, Reston, Virginia 22092, U.S.A. | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/21916/1/0000323.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1016/0021-9614(76)90031-8 | en_US |
dc.identifier.source | The Journal of Chemical Thermodynamics | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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