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dc.contributor.authorOsterkamp, Thomas E.
dc.date.accessioned2024-10-23T20:44:52Z
dc.date.available2024-10-23T20:44:52Z
dc.date.issued1975-04
dc.identifier.urihttp://hdl.handle.net/11122/15537
dc.descriptionUAG R-234; Alaska Sea Grant Report No. 75-3; Scientific Report; Summary: The coastal erosion process has been examined for the northern Alaskan coast for the purpose of developing a conceptual model of off-shore permafrost. A series of as many as five stages of coastal erosion, which are characterized by different thermal and chemical boundary conditions, are necessary to describe the physical setting of the offshore permafrost. The seasonal variations of the thermal and chemical boundary conditions are discussed and it is suggested that these varying boundary conditions can be incorporated into a model of offshore permafrost consisting of the generalized transport equations from non-equilibrium thermodynamics, by successive application of the transport equations to the five stages experienced by a vertical soil profile during the erosion process.en_US
dc.description.sponsorshipThis publication is the result of research sponsored by NOAA, Office of Sea Grant, Department of Commerce, under grant number 40-3-158-41 and by the Alaska Oil and Gas Association.en_US
dc.description.tableofcontentsSummary -- Introduction -- Physical setting -- Transport processes -- Some applicable theories -- Developing a model -- Acknowledgements -- References -- List of figures.en_US
dc.language.isoen_USen_US
dc.publisherGeophysical Institute at the University of Alaska Fairbanksen_US
dc.subjectPermafrosten_US
dc.subjectAlaskaen_US
dc.subjectSubmerged landsen_US
dc.subjectBeach erosionen_US
dc.titleA conceptual model of offshore permafrosten_US
dc.typeReporten_US
refterms.dateFOA2024-10-23T20:44:54Z


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