Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii)

In the construction of an earth bed in regions where permafrost ground occurs, one finds instances of the thawing of the frozen base under the fills of slight height as a result of changes in the heat exchange condition (disruptions of vegetative cover, conditions of evaporation, insolation, condens...

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Bibliographic Details
Main Author: Kulikov,Yu. G.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1975
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA003318
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA003318
id ftdtic:ADA003318
record_format openpolar
spelling ftdtic:ADA003318 2023-05-15T16:37:01+02:00 Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii) Kulikov,Yu. G. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1975-01 text/html http://www.dtic.mil/docs/citations/ADA003318 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA003318 en eng http://www.dtic.mil/docs/citations/ADA003318 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Civil Engineering *PERMAFROST *DAMS HEAT TRANSFER USSR THICKNESS DEPTH GROUND WATER SOILS FREEZING CONSTRUCTION MELTING SURFACE WATERS TRANSLATIONS EARTH FILLS Frozen soils *Earth dams Settlement(Structural) Text 1975 ftdtic 2016-02-20T08:54:41Z In the construction of an earth bed in regions where permafrost ground occurs, one finds instances of the thawing of the frozen base under the fills of slight height as a result of changes in the heat exchange condition (disruptions of vegetative cover, conditions of evaporation, insolation, condensation, albedo of surface) and also as a result of the effect exerted by the surface and ground water. Under such conditions, for finding the amount of settling of the fills during the planning of an earth bed, it is necessary to calculate the thawing depth of the permafrost base or even to determine the height of fill at which the permafrost ground does not thaw. Draft trans. of Transportnoe Stroitelstvo (USSR) n10 p35-37 Oct 68. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Civil Engineering
*PERMAFROST
*DAMS
HEAT TRANSFER
USSR
THICKNESS
DEPTH
GROUND WATER
SOILS
FREEZING
CONSTRUCTION
MELTING
SURFACE WATERS
TRANSLATIONS
EARTH FILLS
Frozen soils
*Earth dams
Settlement(Structural)
spellingShingle Snow
Ice and Permafrost
Civil Engineering
*PERMAFROST
*DAMS
HEAT TRANSFER
USSR
THICKNESS
DEPTH
GROUND WATER
SOILS
FREEZING
CONSTRUCTION
MELTING
SURFACE WATERS
TRANSLATIONS
EARTH FILLS
Frozen soils
*Earth dams
Settlement(Structural)
Kulikov,Yu. G.
Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii)
topic_facet Snow
Ice and Permafrost
Civil Engineering
*PERMAFROST
*DAMS
HEAT TRANSFER
USSR
THICKNESS
DEPTH
GROUND WATER
SOILS
FREEZING
CONSTRUCTION
MELTING
SURFACE WATERS
TRANSLATIONS
EARTH FILLS
Frozen soils
*Earth dams
Settlement(Structural)
description In the construction of an earth bed in regions where permafrost ground occurs, one finds instances of the thawing of the frozen base under the fills of slight height as a result of changes in the heat exchange condition (disruptions of vegetative cover, conditions of evaporation, insolation, condensation, albedo of surface) and also as a result of the effect exerted by the surface and ground water. Under such conditions, for finding the amount of settling of the fills during the planning of an earth bed, it is necessary to calculate the thawing depth of the permafrost base or even to determine the height of fill at which the permafrost ground does not thaw. Draft trans. of Transportnoe Stroitelstvo (USSR) n10 p35-37 Oct 68.
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
format Text
author Kulikov,Yu. G.
author_facet Kulikov,Yu. G.
author_sort Kulikov,Yu. G.
title Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii)
title_short Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii)
title_full Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii)
title_fullStr Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii)
title_full_unstemmed Optimal Height of a Dam for Preservation of Bearing Ground in a Frozen State (Optimalbnaya Vbisota Nasypi dlya Sokhraneniya Grunta Osnovaniya v Merzlom Sostoyanii)
title_sort optimal height of a dam for preservation of bearing ground in a frozen state (optimalbnaya vbisota nasypi dlya sokhraneniya grunta osnovaniya v merzlom sostoyanii)
publishDate 1975
url http://www.dtic.mil/docs/citations/ADA003318
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA003318
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA003318
op_rights APPROVED FOR PUBLIC RELEASE
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