An Approximate Method of Calculating the Temperature Steady State of Water-Permeable Dams (Privlizhennyy Sposov Rascheta Statsionarnogo Temperaturnogo Sostoyaniya fil'Truyushchikh Plotin)

In permafrost areas, in addition to water in permeable dams, use is made of water permeable ones. The thermal conditions of these dams have been fairly studied under the conditions of the planar problem. On the basis of the functions available for determining the temperature steady state of water-pe...

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Bibliographic Details
Main Author: Stavrovskiy,A P
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1977
Subjects:
Snow
Ice and Permafrost
Civil Engineering
*COLD REGIONS
*CONSTRUCTION
*DAMS
HEAT TRANSFER
USSR
STEADY STATE
TEMPERATURE
PERMEABILITY
SOILS
PROFILES
FREEZING
TRANSLATIONS
HYDRODYNAMICS
FILTRATION
PERMAFROST
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/ADA037653
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA037653
Description
Summary:In permafrost areas, in addition to water in permeable dams, use is made of water permeable ones. The thermal conditions of these dams have been fairly studied under the conditions of the planar problem. On the basis of the functions available for determining the temperature steady state of water-permeable dams, this paper proposes dependencies, utilizing N.K. Girinskiy's hydrodynamic functions. (Author) Trans. of unidentified Russian language report p145-153.

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