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Crystal structure of naturally occurring mercury(II) amidonitrate

dc.contributor.authorRandall, Charles J.en_US
dc.contributor.authorPeacor, Donald R.en_US
dc.contributor.authorRouse, Roland C.en_US
dc.contributor.authorDunn, Pete J.en_US
dc.date.accessioned2006-04-07T17:52:26Z
dc.date.available2006-04-07T17:52:26Z
dc.date.issued1982-05en_US
dc.identifier.citationRandall, Charles J., Peacor, Donald R., Rouse, Roland C., Dunn, Pete J. (1982/05)."Crystal structure of naturally occurring mercury(II) amidonitrate." Journal of Solid State Chemistry 42(3): 221-226. <http://hdl.handle.net/2027.42/23994>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6WM2-4BK9W3B-4H/2/155475c3c10f695d17d47cabb8ebae78en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/23994
dc.description.abstractA naturally-occurring mercuroammonium compound from Pitkin County, Colorado, is shown to be the natural analog of synthetic HgNH2NO3. The crystals are isometric, P4132 or P4332, with a = 10.254(1)A and twelve formula weights per cell. Using 437 symmetry-independent reflections, the crystal structure was partially determined and refined to a residual of 0.090. The positions of the Hg atoms and the N and O atoms of the nitrate group were determined, but the amide ion could not be located, probably due to positional disorder. The structure contains mercury atoms arranged in equilateral triangles 3.421(1) A on a side. These triangles are linked through shared vertices into helical chains wound around the fourfold screw axes. Similar triangular units occur in other inorganic Hg(II) compounds. The distortion of the nitrate ion from trigonal planar symmetry is also discussed.en_US
dc.format.extent482458 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleCrystal structure of naturally occurring mercury(II) amidonitrateen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelMaterials Science and Engineeringen_US
dc.subject.hlbsecondlevelChemistryen_US
dc.subject.hlbsecondlevelChemical Engineeringen_US
dc.subject.hlbtoplevelScienceen_US
dc.subject.hlbtoplevelEngineeringen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA; Department of Mineral Sciences, Smithsonian Institution, Washington, D.C. 20560, USAen_US
dc.contributor.affiliationumDepartment of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA; Department of Mineral Sciences, Smithsonian Institution, Washington, D.C. 20560, USAen_US
dc.contributor.affiliationumDepartment of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA; Department of Mineral Sciences, Smithsonian Institution, Washington, D.C. 20560, USAen_US
dc.contributor.affiliationumDepartment of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA; Department of Mineral Sciences, Smithsonian Institution, Washington, D.C. 20560, USAen_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/23994/1/0000243.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0022-4596(82)90001-9en_US
dc.identifier.sourceJournal of Solid State Chemistryen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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