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Compression of klockmannite, CuSe

dc.contributor.authorPeiris, Suhithi M.en_US
dc.contributor.authorPearson, Tania T.en_US
dc.contributor.authorHeinz, Dion L.en_US
dc.date.accessioned2010-05-06T22:51:04Z
dc.date.available2010-05-06T22:51:04Z
dc.date.issued1998-07-08en_US
dc.identifier.citationPeiris, Suhithi M.; Pearson, Tania T.; Heinz, Dion L. (1998). "Compression of klockmannite, CuSe." The Journal of Chemical Physics 109(2): 634-636. <http://hdl.handle.net/2027.42/70875>en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/70875
dc.description.abstractCopper selenide (CuSe) was compressed in a diamond anvil cell at room temperature up to a pressure of 52 GPa and studied using energy dispersive x-ray diffraction and Raman spectroscopy. CuSe is nearly isostructural with copper sulfide (CuS), and a previous study indicates that copper sulfide undergoes reversible pressure-induced amorphization at 18 GPa. The intensity of the x-ray diffraction peaks for CuSe decrease slowly, however, they never completely disappear up to a pressure of 52 GPa. The third-order Birch–Murnaghan equation of state fit to the data yields K0 = 96.9±5.3 GPaK0=96.9±5.3GPa and K0′ = 4.1±0.5.K0′=4.1±0.5. Vinet’s universal equation of state yields essentially identical parameters. Raman spectroscopy demonstrates that upon compression, the S–S bond in CuS compresses differently than the Se–Se bond in CuSe, possibly accounting for the different high pressure behavior of these two very similar compounds. © 1998 American Institute of Physics.en_US
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dc.publisherThe American Institute of Physicsen_US
dc.rights© The American Institute of Physicsen_US
dc.titleCompression of klockmannite, CuSeen_US
dc.typeArticleen_US
dc.subject.hlbsecondlevelPhysicsen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Chemistry, University of Michigan, Ann Arbor, Michigan 48109en_US
dc.contributor.affiliationotherDepartment of Chemistry, University of Chicago, Chicago, Illinois 60637en_US
dc.contributor.affiliationotherDepartment of Geophysical Sciences and James Franck Institute, University of Chicago, Chicago, Illinois 60637en_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/70875/2/JCPSA6-109-2-634-1.pdf
dc.identifier.doi10.1063/1.476601en_US
dc.identifier.sourceThe Journal of Chemical Physicsen_US
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dc.identifier.citedreferenceS. M. Peiris, Ph.D. dissertation, University of Chicago, 1996.en_US
dc.owningcollnamePhysics, Department of


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