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dc.contributor.authorKane, D. L.
dc.date.accessioned2012-12-11T19:50:28Z
dc.date.available2012-12-11T19:50:28Z
dc.date.issued1975-12
dc.identifier.urihttp://hdl.handle.net/11122/1194
dc.description.abstractThe movement of soil moisture through cold regions soils is an active process that continues throughout the year. It represents one mechanism of heat transport in subsurface soil, conduction being the main mode of heat flow. In frozen soils, this moisture may undergo phase change resulting in two significant events: 1. deformation of the near-surface layer, and 2. liberation or uptake of heat at the point of phase change. Where deformation (induced by either frost heaving or thaw consolidation) occurs in man-made embankments, it is readily apparent at the surface. Restoration of the deformed surface requires large sums of money.en_US
dc.description.sponsorshipOWRR CONTRACT NO. 14-31-0001-5002 GRANT NO. A-053-ALAS. The work upon which this completion report is based was supported by funds provided by the U. S. Department of Interior, Office of Water Research and Technology, as authorized under the Water Resources Research Act of 1964, Public Law 88-379, as amended.en_US
dc.publisherUniversity of Alaska, Institute of Water Resourcesen_US
dc.relation.ispartofseriesIWR;no. 70
dc.titleWinter soil water dynamics: Completion reporten_US
dc.typeTechnical Reporten_US
refterms.dateFOA2020-01-24T14:56:19Z


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