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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Format: | Article |
Language: | Russian |
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V.V. Dokuchaev Soil Science Institute
2014-04-01
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Series: | Бюллетень Почвенного института им. В.В. Докучаева |
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Online Access: | https://bulletin.esoil.ru/jour/article/view/282 |
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author | D. A. Kaverin A. V. Pastukhov G. G. Mazhitova |
author_facet | D. A. Kaverin A. V. Pastukhov G. G. Mazhitova |
author_sort | D. A. Kaverin |
collection | DOAJ |
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. |
first_indexed | 2024-03-08T19:15:07Z |
format | Article |
id | doaj.art-025e5c5d965b4511a1399171c4c73667 |
institution | Directory Open Access Journal |
issn | 0136-1694 2312-4202 |
language | Russian |
last_indexed | 2024-04-24T15:44:27Z |
publishDate | 2014-04-01 |
publisher | V.V. Dokuchaev Soil Science Institute |
record_format | Article |
series | Бюллетень Почвенного института им. В.В. Докучаева |
spelling | doaj.art-025e5c5d965b4511a1399171c4c736672024-04-01T16:06:44ZrusV.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 |
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 |
title | 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_short | 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 |
topic | temperature regime cold frozen soils permafrost-affected rocks seasonal-thawing layer |
url | https://bulletin.esoil.ru/jour/article/view/282 |
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