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...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1975
|
Subjects: | |
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 |