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...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1975
|
Subjects: | |
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 |
_version_ |
1766027320346279936 |