PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA

PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA

Under study was the temperature regime of frozen soils situated along the southern boundary of cryolithozone in the North-East of European Russia. In southern tundra the frozen soils with the cold temperature regime are confined to peat and mineral parent materials. The seasonal and long-term temper...

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Main Authors: D. A. Kaverin, A. V. Pastukhov, G. G. Mazhitova
Format: Article
Language:Russian
Published: V.V. Dokuchaev Soil Science Institute 2014-04-01
Series:Бюллетень Почвенного института им. В.В. Докучаева
Subjects:
temperature regime
cold frozen soils
permafrost-affected rocks
seasonal-thawing layer
Online Access:https://bulletin.esoil.ru/jour/article/view/282
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spelling doaj-025e5c5d965b4511a1399171c4c736672021-07-28T13:05:28ZrusV.V. Dokuchaev Soil Science InstituteБюллетень Почвенного института им. В.В. Докучаева0136-16942312-42022014-04-01075486210.19047/0136-1694-2014-75-48-62281PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIAD. A. Kaverin0A. V. Pastukhov1G. G. Mazhitova2Institute of Biology, Komi Scientific Center, Ural Branch of the Russian Academy of SciencesInstitute of Biology, Komi Scientific Center, Ural Branch of the Russian Academy of SciencesInstitute of Biology, Komi Scientific Center, Ural Branch of the Russian Academy of SciencesUnder study was the temperature regime of frozen soils situated along the southern boundary of cryolithozone in the North-East of European Russia. In southern tundra the frozen soils with the cold temperature regime are confined to peat and mineral parent materials. The seasonal and long-term temperature dynamics in seasonal-thawing and underlying permafrost-affected layer is shown. The frozen soils are characterized by the main temperature indices.https://bulletin.esoil.ru/jour/article/view/282temperature regimecold frozen soilspermafrost-affected rocksseasonal-thawing layer
collection DOAJ
language Russian
format Article
sources DOAJ
author D. A. Kaverin
A. V. Pastukhov
G. G. Mazhitova
spellingShingle D. A. Kaverin
A. V. Pastukhov
G. G. Mazhitova
PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA
Бюллетень Почвенного института им. В.В. Докучаева
temperature regime
cold frozen soils
permafrost-affected rocks
seasonal-thawing layer
author_facet D. A. Kaverin
A. V. Pastukhov
G. G. Mazhitova
author_sort D. A. Kaverin
title PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA
title_short PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA
title_full PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA
title_fullStr PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA
title_full_unstemmed PECULIAR TEMPERATURE REGIME IN COLD FROZEN SOILS ALONG THE SOUTHERN BOUNDARY OF THE CRYOLITHOZONE IN THE NORTH-EAST OF EUROPEAN RUSSIA
title_sort peculiar temperature regime in cold frozen soils along the southern boundary of the cryolithozone in the north-east of european russia
publisher V.V. Dokuchaev Soil Science Institute
series Бюллетень Почвенного института им. В.В. Докучаева
issn 0136-1694
2312-4202
publishDate 2014-04-01
description Under study was the temperature regime of frozen soils situated along the southern boundary of cryolithozone in the North-East of European Russia. In southern tundra the frozen soils with the cold temperature regime are confined to peat and mineral parent materials. The seasonal and long-term temperature dynamics in seasonal-thawing and underlying permafrost-affected layer is shown. The frozen soils are characterized by the main temperature indices.
topic temperature regime
cold frozen soils
permafrost-affected rocks
seasonal-thawing layer
url https://bulletin.esoil.ru/jour/article/view/282
work_keys_str_mv AT dakaverin peculiartemperatureregimeincoldfrozensoilsalongthesouthernboundaryofthecryolithozoneinthenortheastofeuropeanrussia
AT avpastukhov peculiartemperatureregimeincoldfrozensoilsalongthesouthernboundaryofthecryolithozoneinthenortheastofeuropeanrussia
AT ggmazhitova peculiartemperatureregimeincoldfrozensoilsalongthesouthernboundaryofthecryolithozoneinthenortheastofeuropeanrussia
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