HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA
The results of hydrological survey of the largest lakes of the Yamal Peninsula – Neyto 1st, Neyto-Erto, Neyto-Malto, Yambuto and Yarato 2 nd , undertaken in September 2007 are presented. The morphometric characteristics of these lakes as well as the hydrological properties of their water at the end...
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ftdoajarticles:oai:doaj.org/article:cbe7c955301d4cb193c3eb6e490037e5 2023-05-15T18:45:32+02:00 HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA Konstantin Edelstein Andrei Alabyan Sergei Gorin Artem Popryadukhin 2017-10-01T00:00:00Z https://doi.org/10.17076/lim571 https://doaj.org/article/cbe7c955301d4cb193c3eb6e490037e5 EN RU eng rus Karelian Research Centre of the Russian Academy of Sciences http://journals.krc.karelia.ru/index.php/limnology/article/view/571 https://doaj.org/toc/1997-3217 https://doaj.org/toc/2312-4504 1997-3217 2312-4504 doi:10.17076/lim571 https://doaj.org/article/cbe7c955301d4cb193c3eb6e490037e5 Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Iss 10, Pp 3-16 (2017) hydrological regime morphometry mineralization temperature chemical composition of water neyto yambuto yarato yamal Science Q article 2017 ftdoajarticles https://doi.org/10.17076/lim571 2022-12-31T11:04:59Z The results of hydrological survey of the largest lakes of the Yamal Peninsula – Neyto 1st, Neyto-Erto, Neyto-Malto, Yambuto and Yarato 2 nd , undertaken in September 2007 are presented. The morphometric characteristics of these lakes as well as the hydrological properties of their water at the end of the autumn low water stage were determined. Many of the largest lakes of Yamal have a complex bottom topography due to the presence of cryptodepressions cutting deeply into the bottom. They are both shallow lakes with an average depth less than3 m and lakes with average depths exceeding 10–20 m. There is thorough vertical mixing of the water masses (even in deep-water hollows) due to the impact of wind and convection. Extremely low mineralization and very low content of hydrocarbonates in the water result from the dominance of atmospheric precipitation in the input part of the lake water balance. Greenish coloring of water in some of the surveyed lakes and moderate supersaturation with oxygen in all the lakes evidence a considerable development of cold-loving phytoplankton species (during the growing season it is promoted by a longer daylight duration). Article in Journal/Newspaper Yamal Peninsula Directory of Open Access Journals: DOAJ Articles Yamal Peninsula ENVELOPE(69.873,69.873,70.816,70.816) Proceedings of the Karelian Research Centre of the Russian Academy of Sciences 10 3 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Russian |
topic |
hydrological regime morphometry mineralization temperature chemical composition of water neyto yambuto yarato yamal Science Q |
spellingShingle |
hydrological regime morphometry mineralization temperature chemical composition of water neyto yambuto yarato yamal Science Q Konstantin Edelstein Andrei Alabyan Sergei Gorin Artem Popryadukhin HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA |
topic_facet |
hydrological regime morphometry mineralization temperature chemical composition of water neyto yambuto yarato yamal Science Q |
description |
The results of hydrological survey of the largest lakes of the Yamal Peninsula – Neyto 1st, Neyto-Erto, Neyto-Malto, Yambuto and Yarato 2 nd , undertaken in September 2007 are presented. The morphometric characteristics of these lakes as well as the hydrological properties of their water at the end of the autumn low water stage were determined. Many of the largest lakes of Yamal have a complex bottom topography due to the presence of cryptodepressions cutting deeply into the bottom. They are both shallow lakes with an average depth less than3 m and lakes with average depths exceeding 10–20 m. There is thorough vertical mixing of the water masses (even in deep-water hollows) due to the impact of wind and convection. Extremely low mineralization and very low content of hydrocarbonates in the water result from the dominance of atmospheric precipitation in the input part of the lake water balance. Greenish coloring of water in some of the surveyed lakes and moderate supersaturation with oxygen in all the lakes evidence a considerable development of cold-loving phytoplankton species (during the growing season it is promoted by a longer daylight duration). |
format |
Article in Journal/Newspaper |
author |
Konstantin Edelstein Andrei Alabyan Sergei Gorin Artem Popryadukhin |
author_facet |
Konstantin Edelstein Andrei Alabyan Sergei Gorin Artem Popryadukhin |
author_sort |
Konstantin Edelstein |
title |
HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA |
title_short |
HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA |
title_full |
HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA |
title_fullStr |
HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA |
title_full_unstemmed |
HYDROLOGICAL AND HYDROCHEMICAL FEATURES OF THE LARGEST LAKES OF THE YAMAL PENINSULA |
title_sort |
hydrological and hydrochemical features of the largest lakes of the yamal peninsula |
publisher |
Karelian Research Centre of the Russian Academy of Sciences |
publishDate |
2017 |
url |
https://doi.org/10.17076/lim571 https://doaj.org/article/cbe7c955301d4cb193c3eb6e490037e5 |
long_lat |
ENVELOPE(69.873,69.873,70.816,70.816) |
geographic |
Yamal Peninsula |
geographic_facet |
Yamal Peninsula |
genre |
Yamal Peninsula |
genre_facet |
Yamal Peninsula |
op_source |
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Iss 10, Pp 3-16 (2017) |
op_relation |
http://journals.krc.karelia.ru/index.php/limnology/article/view/571 https://doaj.org/toc/1997-3217 https://doaj.org/toc/2312-4504 1997-3217 2312-4504 doi:10.17076/lim571 https://doaj.org/article/cbe7c955301d4cb193c3eb6e490037e5 |
op_doi |
https://doi.org/10.17076/lim571 |
container_title |
Proceedings of the Karelian Research Centre of the Russian Academy of Sciences |
container_issue |
10 |
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3 |
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1766236619516411904 |