Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/9540
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dc.contributorNational Science Foundation (U.S.). Division of Polar Programs-
dc.contributorUnited States. Naval Undersea Center-
dc.contributorState University of New York at Buffalo. Department of Geology-
dc.contributorSan Diego State University-
dc.contributor.authorHerron, M. M.-
dc.contributor.authorLangway, Chester C., 1929--
dc.contributor.authorWeiss, H. V.-
dc.contributor.authorHurley, J. P.-
dc.contributor.authorKerr, R. J.-
dc.contributor.authorCragin, James H.-
dc.date.accessioned2016-06-20T13:42:21Z-
dc.date.available2016-06-20T13:42:21Z-
dc.date.issued1976-07-
dc.identifier.urihttp://hdl.handle.net/11681/9540-
dc.descriptionCRREL Report-
dc.descriptionAbstract: Chemical analysis of surface snows and deeper ice core samples from Milcent, Greenland, indicates a marine origin for Na and Cl and a terrestrial origin for Al, Mn and V. Pre-1900 enrichment factors, based on average crustal composition, are high for Zn and Hg and appear to be related to their volatility. A comparison of pre-1900 and 1971-1973 concentrations of V and Hg shows no decided increase from industrial production; however, the abundance of Zn (relative to Al) increased three-fold during this time period. The chemical composition of ancient ice is extemely useful in interpreting modern aerosols.-
dc.publisherCold Regions Research and Engineering Laboratory (U.S.)-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1011470-
dc.relation.ispartofseriesCRREL report ; 76-24.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectAnnual accumulations-
dc.subjectIce-
dc.subjectChemical analysis-
dc.subjectIce cores-
dc.subjectDating-
dc.subjectSeasonal variations-
dc.subjectGreenland-
dc.subjectVanadium-
dc.titleVanadium and other elements in Greenland ice cores-
dc.typeReporten_US
Appears in Collections:CRREL Report

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