Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya)
The report is devoted to the study of the seasonal thawing os soil and its relationship with the temperature, soil moistness, and meteorological conditions. The territory under study comprises a plains sector in the interfluve of the Ob' River and its tributary, the Poly'ye, formed of sand...
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ftdtic:AD0753035 2023-05-15T15:03:25+02:00 Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya) Dyakonov,K. N. Reteyum,A. Yu. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1972-11 text/html http://www.dtic.mil/docs/citations/AD0753035 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0753035 en eng http://www.dtic.mil/docs/citations/AD0753035 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Soil Mechanics Snow Ice and Permafrost (*PERMAFROST SOILS) (*SOILS ARCTIC REGIONS) MELTING FREEZING RIVERS SWAMPS MOISTURE METEOROLOGICAL PHENOMENA PLANTS(BOTANY) TEMPERATURE INTERACTIONS ICE FORESTRY USSR FOREST LAND *FREEZING *SOILS TRANSLATIONS *TUNDRA Text 1972 ftdtic 2016-02-19T02:19:33Z The report is devoted to the study of the seasonal thawing os soil and its relationship with the temperature, soil moistness, and meteorological conditions. The territory under study comprises a plains sector in the interfluve of the Ob' River and its tributary, the Poly'ye, formed of sands and sandy-loamy fluvioglacial deposits. The texture of the latter is uniform. All of the natural territorial complexes in the interfluve are supported by frozen layers with a depth of 200-300 m. The observations were conducted in five different natural complexes geochemically interconnected and differing in altitude and moisture conditions. (Author) Draft trans. of Geograficheskie Soobshcheniya (USSR) n3 p59-62 1966. Text Arctic Ice ob river permafrost Tundra Defense Technical Information Center: DTIC Technical Reports database Arctic |
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 (*PERMAFROST SOILS) (*SOILS ARCTIC REGIONS) MELTING FREEZING RIVERS SWAMPS MOISTURE METEOROLOGICAL PHENOMENA PLANTS(BOTANY) TEMPERATURE INTERACTIONS ICE FORESTRY USSR FOREST LAND *FREEZING *SOILS TRANSLATIONS *TUNDRA |
spellingShingle |
Soil Mechanics Snow Ice and Permafrost (*PERMAFROST SOILS) (*SOILS ARCTIC REGIONS) MELTING FREEZING RIVERS SWAMPS MOISTURE METEOROLOGICAL PHENOMENA PLANTS(BOTANY) TEMPERATURE INTERACTIONS ICE FORESTRY USSR FOREST LAND *FREEZING *SOILS TRANSLATIONS *TUNDRA Dyakonov,K. N. Reteyum,A. Yu. Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya) |
topic_facet |
Soil Mechanics Snow Ice and Permafrost (*PERMAFROST SOILS) (*SOILS ARCTIC REGIONS) MELTING FREEZING RIVERS SWAMPS MOISTURE METEOROLOGICAL PHENOMENA PLANTS(BOTANY) TEMPERATURE INTERACTIONS ICE FORESTRY USSR FOREST LAND *FREEZING *SOILS TRANSLATIONS *TUNDRA |
description |
The report is devoted to the study of the seasonal thawing os soil and its relationship with the temperature, soil moistness, and meteorological conditions. The territory under study comprises a plains sector in the interfluve of the Ob' River and its tributary, the Poly'ye, formed of sands and sandy-loamy fluvioglacial deposits. The texture of the latter is uniform. All of the natural territorial complexes in the interfluve are supported by frozen layers with a depth of 200-300 m. The observations were conducted in five different natural complexes geochemically interconnected and differing in altitude and moisture conditions. (Author) Draft trans. of Geograficheskie Soobshcheniya (USSR) n3 p59-62 1966. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H |
format |
Text |
author |
Dyakonov,K. N. Reteyum,A. Yu. |
author_facet |
Dyakonov,K. N. Reteyum,A. Yu. |
author_sort |
Dyakonov,K. N. |
title |
Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya) |
title_short |
Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya) |
title_full |
Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya) |
title_fullStr |
Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya) |
title_full_unstemmed |
Active Layer Dynamics in Tundra and Forest Tundra of Lower Ob Region (Dinamika Sezonnotaloga Sloya v Tundre i Lesotundre Nezhnego Priobya) |
title_sort |
active layer dynamics in tundra and forest tundra of lower ob region (dinamika sezonnotaloga sloya v tundre i lesotundre nezhnego priobya) |
publishDate |
1972 |
url |
http://www.dtic.mil/docs/citations/AD0753035 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0753035 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Ice ob river permafrost Tundra |
genre_facet |
Arctic Ice ob river permafrost Tundra |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0753035 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766335277174882304 |