Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/11992
Full metadata record
DC FieldValueLanguage
dc.contributor.authorOliphant, Joseph L.-
dc.contributor.authorTice, A. R. (Allen R.)-
dc.date.accessioned2016-06-20T14:27:44Z-
dc.date.available2016-06-20T14:27:44Z-
dc.date.issued1984-09-
dc.identifier.urihttp://hdl.handle.net/11681/11992-
dc.descriptionSpecial Report-
dc.descriptionAbstract: An experiment was performed to determine the rate of equilibration of deuterium between the ice and liquid phases of water in partially frozen soil. The results of this experiment are consistent with a diffusion rate of deuterium in ice of 1 or 2x10(-10) cm(2)/s. A method for calculating the approximate equilibration time, given the size of the ice crystals in the system, is provided. This calculation compares well with the experimental results. Note: (-10) is an exponent for scientific notation. (2) indicates cm is squared.-
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/1010862-
dc.relation.ispartofseriesSpecial report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 84-27.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectDeuterium-
dc.subjectFrozen soil-
dc.subjectLaboratory tests-
dc.subjectTracer studies-
dc.subjectWater migration-
dc.titleDeuterium diffusion in a soil-water-ice mixture-
dc.typeReporten_US
Appears in Collections:Special Report

Files in This Item:
File Description SizeFormat 
SR-84-27.pdf564.62 kBAdobe PDFThumbnail
View/Open