Variation in Thickness and Temperature Regime of Permafrost beneath Areas of Sediment Accumulation and Denudation (Izmenenie Moshchnosti i Temperaturnogo Rezhima Mnogoletnemerzlykh Porod v Usloviyakh Osadkonakopleniya i Denudatsii)

The report discusses an approximate solution to the question concerning the dynamics of the frozen soil layer under conditions of sediment accumulation. Draft trans. of mono. Eksperimentalnye Issledovaniya Protsessov Teploobmena v Merzlykh Gornykh Porodakh (Experimental Studies of Heat Exchange Proc...

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Bibliographic Details
Main Author: Balobaev,V. T.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1973
Subjects:
Snow
Ice and Permafrost
*PERMAFROST
THERMAL PROPERTIES
THICKNESS
FREEZING
SOILS
GRADIENTS
TEMPERATURE
DISPLACEMENT
GEOLOGY
ROCK
MELTING
APPROXIMATION(MATHEMATICS)
TRANSLATIONS
USSR
Frozen soils
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/AD0769722
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0769722
Description
Summary:The report discusses an approximate solution to the question concerning the dynamics of the frozen soil layer under conditions of sediment accumulation. Draft trans. of mono. Eksperimentalnye Issledovaniya Protsessov Teploobmena v Merzlykh Gornykh Porodakh (Experimental Studies of Heat Exchange Processes in Frozen Rocks) Moscow, 1972 p101-108.

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