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)

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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Bibliographische Detailangaben
1. Verfasser: Balobaev,V T
Format: Report
Sprache:eng
Schlagworte:
APPROXIMATION(MATHEMATICS)
DISPLACEMENT
FREEZING
Frozen soils
GEOLOGY
GRADIENTS
MELTING
PERMAFROST
ROCK
Snow, Ice and Permafrost
SOILS
TEMPERATURE
THERMAL PROPERTIES
THICKNESS
TRANSLATIONS
USSR
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Beschreibung
Zusammenfassung: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.