Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits

In the northern regions of the USSR, a group of structures called earth beds are being developed. A compilation of forecasts indicating the variation in permafrost ground under fills and in excavations has rarely been made by calculation until now, because in each case, it is necessary to solve a tw...

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Bibliographic Details
Main Author: Zamolotchikova,S. A.
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/ADA003209
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA003209
id ftdtic:ADA003209
record_format openpolar
spelling ftdtic:ADA003209 2023-05-15T16:36:53+02:00 Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits Zamolotchikova,S. A. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1975-02 text/html http://www.dtic.mil/docs/citations/ADA003209 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA003209 en eng http://www.dtic.mil/docs/citations/ADA003209 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost Civil Engineering *PERMAFROST *EARTH FILLS THERMAL PROPERTIES USSR TEMPERATURE DEFORMATION FREEZING MATHEMATICAL PREDICTION STRUCTURAL RESPONSE MELTING TRANSLATIONS EMBANKMENTS FROST HEAVE Earth dams Settlement(Structural) Text 1975 ftdtic 2016-02-20T08:54:00Z In the northern regions of the USSR, a group of structures called earth beds are being developed. A compilation of forecasts indicating the variation in permafrost ground under fills and in excavations has rarely been made by calculation until now, because in each case, it is necessary to solve a two- or three-dimensional problem regarding the freeze-thaw cycles in soils. A prediction of the variation in permafrost conditions beneath fills can now be formulated based on the results of interdisciplinary permafrost surveying. This report discusses one of the first attempts at analyzing the influence of cutoff temperatures on the variation in permafrost ground under a fill. Draft trans. of Merzlotnye Issledovaniya (USSR) n8 p186-198 1968. 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 Soil Mechanics
Snow
Ice and Permafrost
Civil Engineering
*PERMAFROST
*EARTH FILLS
THERMAL PROPERTIES
USSR
TEMPERATURE
DEFORMATION
FREEZING
MATHEMATICAL PREDICTION
STRUCTURAL RESPONSE
MELTING
TRANSLATIONS
EMBANKMENTS
FROST HEAVE
Earth dams
Settlement(Structural)
spellingShingle Soil Mechanics
Snow
Ice and Permafrost
Civil Engineering
*PERMAFROST
*EARTH FILLS
THERMAL PROPERTIES
USSR
TEMPERATURE
DEFORMATION
FREEZING
MATHEMATICAL PREDICTION
STRUCTURAL RESPONSE
MELTING
TRANSLATIONS
EMBANKMENTS
FROST HEAVE
Earth dams
Settlement(Structural)
Zamolotchikova,S. A.
Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits
topic_facet Soil Mechanics
Snow
Ice and Permafrost
Civil Engineering
*PERMAFROST
*EARTH FILLS
THERMAL PROPERTIES
USSR
TEMPERATURE
DEFORMATION
FREEZING
MATHEMATICAL PREDICTION
STRUCTURAL RESPONSE
MELTING
TRANSLATIONS
EMBANKMENTS
FROST HEAVE
Earth dams
Settlement(Structural)
description In the northern regions of the USSR, a group of structures called earth beds are being developed. A compilation of forecasts indicating the variation in permafrost ground under fills and in excavations has rarely been made by calculation until now, because in each case, it is necessary to solve a two- or three-dimensional problem regarding the freeze-thaw cycles in soils. A prediction of the variation in permafrost conditions beneath fills can now be formulated based on the results of interdisciplinary permafrost surveying. This report discusses one of the first attempts at analyzing the influence of cutoff temperatures on the variation in permafrost ground under a fill. Draft trans. of Merzlotnye Issledovaniya (USSR) n8 p186-198 1968.
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
format Text
author Zamolotchikova,S. A.
author_facet Zamolotchikova,S. A.
author_sort Zamolotchikova,S. A.
title Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits
title_short Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits
title_full Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits
title_fullStr Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits
title_full_unstemmed Variation of Geocryological Conditions Beneath Dams Depending on Upper Temperature Limits
title_sort variation of geocryological conditions beneath dams depending on upper temperature limits
publishDate 1975
url http://www.dtic.mil/docs/citations/ADA003209
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA003209
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA003209
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027203581050880