Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia
The work is devoted to results of study the chemical composition of snow in mountain taiga and permafrost landscapes of Yakutia. We studied snow cover in different mountain-belt types of landscapes. The composition and calculated volumes of chemical elements and compounds are studied in snow. The ch...
| Published in: | Ice and Snow |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | Russian |
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IGRAS
2015
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| Online Access: | https://ice-snow.igras.ru/jour/article/view/26 https://doi.org/10.15356/2076-6734-2014-1-73-80 |
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ftjias:oai:oai.ice.elpub.ru:article/26 |
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Open Polar |
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Ice and Snow (E-Journal) |
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ftjias |
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Russian |
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Сryosphere;geochemistry;landscapes;snow cover;Yakutia Геохимия;криосфера;ландшафты;снежный покров;Якутия |
| spellingShingle |
Сryosphere;geochemistry;landscapes;snow cover;Yakutia Геохимия;криосфера;ландшафты;снежный покров;Якутия V. Makarov N. В. Макаров Н. Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia |
| topic_facet |
Сryosphere;geochemistry;landscapes;snow cover;Yakutia Геохимия;криосфера;ландшафты;снежный покров;Якутия |
| description |
The work is devoted to results of study the chemical composition of snow in mountain taiga and permafrost landscapes of Yakutia. We studied snow cover in different mountain-belt types of landscapes. The composition and calculated volumes of chemical elements and compounds are studied in snow. The chemical composition of snow in mountain taiga and permafrost landscape has remained relatively constant (hydrocarbonate chloride-bicarbonate or sodium-calcium, low sulfate content). The dominant influence on the chemical composition of snow at plains and mountain permafrost landscapes has a continental origin, mainly carbon compounds. In mountain desert, where there is predominantly regional transfer, along with the carbon significant role in atmospheric precipitation in cold season belongs to the nitrogen compounds, mainly ammonium. The total density of the entry of soluble and insoluble components in the form of snow decreases regularly with change of altitude. The distribution of trace elements in the snow cover is not a subject to altitudinal zonation. The maximum content of heavy metals (Mn, Cu, Pb, Cd), F, and Sr in the snow cover is observed in the landscapes of mountain woodlands and mountain tundra, where the route crossed research Sette-Daban metallogenic zone of stratiform Cu and Pb-Zn mineralization. Исследован снежный покров в разных типах ландшафтов Якутии. Установлено, что химический состав снега таёжных и горных мерзлотных ландшафтов хлоридно-гидрокарбонатный или гидрокарбонатный натриево-кальциевый с небольшим содержанием сульфатов. Преобладающее влияние на формирование химического состава снега оказывают соли континентального происхождения, преимущественно соединения углерода. В ландшафтах горных пустынь, где преобладает региональный перенос, наряду с углеродом, значительная роль в атмосферных выпадениях холодного времени года принадлежит аммонийным соединениям азота. Суммарное поступление растворимых и нерастворимых форм компонентов в снежный покров снижается при переходе от равнин к горным ... |
| format |
Article in Journal/Newspaper |
| author |
V. Makarov N. В. Макаров Н. |
| author_facet |
V. Makarov N. В. Макаров Н. |
| author_sort |
V. Makarov N. |
| title |
Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia |
| title_short |
Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia |
| title_full |
Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia |
| title_fullStr |
Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia |
| title_full_unstemmed |
Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia |
| title_sort |
geochemistry of snow cover in taiga and alpine permafrost landscapes in yakutia |
| publisher |
IGRAS |
| publishDate |
2015 |
| url |
https://ice-snow.igras.ru/jour/article/view/26 https://doi.org/10.15356/2076-6734-2014-1-73-80 |
| genre |
permafrost taiga Tundra Yakutia Якути* Якутия |
| genre_facet |
permafrost taiga Tundra Yakutia Якути* Якутия |
| op_source |
Ice and Snow; Том 54, № 1 (2014); 73-80 Лёд и Снег; Том 54, № 1 (2014); 73-80 2412-3765 2076-6734 10.15356/2076-6734-2014-1 |
| op_relation |
Vasilenko V.N., Nazarov I.M., Fridman Sh.D. Monitoring zagryazneniya snezhnogo pokrova. Monitoring of snow cover contamination. Leningrad: Hydrometeoizdat, 1985: 182 p. [In Russian]. Iveronova M.I. Evaporation from snow cover in Terskey Alatau Range in winter 1958/59. Meteorologiya i gidrologiya. Meteorology and Hydrology. 1961, 2: 24–25. [In Russian]. Kazurova N.S. Synoptic processes in Yakutia in different seasons and their short characteristics. General information. Voprosy geografii Yakutii. Problems of Yakutia geography. Issue 1. Yakutsk, 1961: 19–26. [In Russian]. Klyukin N.K. Klimaticheskiy ocherk Severo-Vostoka SSSR. Climatic essay of North-East of the USSR. Moscow: Hydrometeoizdat, 1960: 118 p. [In Russian]. Makarov V.N. Fluorine in snow cover in the Lena-Vilyui interfluves. Nauka i obrazovanie. Science and Education. 2003, 3 (31): 65–69. [In Russian]. Makarov V.N., Fedoseev N.F., Fedoseeva V.I. Geochimiya snezhnogo pokrova Yakutii. Geochemistry of snow cover in Yakutia. Yakutsk: Institute of Permafrost, Siberian Branch of the Russian Academy of Sciences, 1990: 152 p. [In Russian]. Merzlotnye landshafty Yakutii. Permafrost landscapes of Yakutia. Explanation to the map of scale1:2 500 000. Novosibirsk: GUGK, 1989: 170 p. [In Russian]. Skachkov Yu.B. Trends of changes in extreme of air temperature in Yakutsk city. Nauka i obrazovanie. Science and Education. 2012, 3 (66): 39–41. [In Russian]. https://ice-snow.igras.ru/jour/article/view/26 doi:10.15356/2076-6734-2014-1-73-80 |
| op_rights |
Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access). Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). |
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https://doi.org/10.15356/2076-6734-2014-1-73-80 https://doi.org/10.15356/2076-6734-2014-1 |
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ftjias:oai:oai.ice.elpub.ru:article/26 2023-05-15T17:57:08+02:00 Geochemistry of snow cover in taiga and alpine permafrost landscapes in Yakutia Геохимия снежного покрова таёжных и горных мерзлотных ландшафтов Якутии V. Makarov N. В. Макаров Н. 2015-03-25 https://ice-snow.igras.ru/jour/article/view/26 https://doi.org/10.15356/2076-6734-2014-1-73-80 ru rus IGRAS Vasilenko V.N., Nazarov I.M., Fridman Sh.D. Monitoring zagryazneniya snezhnogo pokrova. Monitoring of snow cover contamination. Leningrad: Hydrometeoizdat, 1985: 182 p. [In Russian]. Iveronova M.I. Evaporation from snow cover in Terskey Alatau Range in winter 1958/59. Meteorologiya i gidrologiya. Meteorology and Hydrology. 1961, 2: 24–25. [In Russian]. Kazurova N.S. Synoptic processes in Yakutia in different seasons and their short characteristics. General information. Voprosy geografii Yakutii. Problems of Yakutia geography. Issue 1. Yakutsk, 1961: 19–26. [In Russian]. Klyukin N.K. Klimaticheskiy ocherk Severo-Vostoka SSSR. Climatic essay of North-East of the USSR. Moscow: Hydrometeoizdat, 1960: 118 p. [In Russian]. Makarov V.N. Fluorine in snow cover in the Lena-Vilyui interfluves. Nauka i obrazovanie. Science and Education. 2003, 3 (31): 65–69. [In Russian]. Makarov V.N., Fedoseev N.F., Fedoseeva V.I. Geochimiya snezhnogo pokrova Yakutii. Geochemistry of snow cover in Yakutia. Yakutsk: Institute of Permafrost, Siberian Branch of the Russian Academy of Sciences, 1990: 152 p. [In Russian]. Merzlotnye landshafty Yakutii. Permafrost landscapes of Yakutia. Explanation to the map of scale1:2 500 000. Novosibirsk: GUGK, 1989: 170 p. [In Russian]. Skachkov Yu.B. Trends of changes in extreme of air temperature in Yakutsk city. Nauka i obrazovanie. Science and Education. 2012, 3 (66): 39–41. [In Russian]. https://ice-snow.igras.ru/jour/article/view/26 doi:10.15356/2076-6734-2014-1-73-80 Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access). Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). CC-BY Ice and Snow; Том 54, № 1 (2014); 73-80 Лёд и Снег; Том 54, № 1 (2014); 73-80 2412-3765 2076-6734 10.15356/2076-6734-2014-1 Сryosphere;geochemistry;landscapes;snow cover;Yakutia Геохимия;криосфера;ландшафты;снежный покров;Якутия info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2014-1-73-80 https://doi.org/10.15356/2076-6734-2014-1 2022-12-20T13:29:44Z The work is devoted to results of study the chemical composition of snow in mountain taiga and permafrost landscapes of Yakutia. We studied snow cover in different mountain-belt types of landscapes. The composition and calculated volumes of chemical elements and compounds are studied in snow. The chemical composition of snow in mountain taiga and permafrost landscape has remained relatively constant (hydrocarbonate chloride-bicarbonate or sodium-calcium, low sulfate content). The dominant influence on the chemical composition of snow at plains and mountain permafrost landscapes has a continental origin, mainly carbon compounds. In mountain desert, where there is predominantly regional transfer, along with the carbon significant role in atmospheric precipitation in cold season belongs to the nitrogen compounds, mainly ammonium. The total density of the entry of soluble and insoluble components in the form of snow decreases regularly with change of altitude. The distribution of trace elements in the snow cover is not a subject to altitudinal zonation. The maximum content of heavy metals (Mn, Cu, Pb, Cd), F, and Sr in the snow cover is observed in the landscapes of mountain woodlands and mountain tundra, where the route crossed research Sette-Daban metallogenic zone of stratiform Cu and Pb-Zn mineralization. Исследован снежный покров в разных типах ландшафтов Якутии. Установлено, что химический состав снега таёжных и горных мерзлотных ландшафтов хлоридно-гидрокарбонатный или гидрокарбонатный натриево-кальциевый с небольшим содержанием сульфатов. Преобладающее влияние на формирование химического состава снега оказывают соли континентального происхождения, преимущественно соединения углерода. В ландшафтах горных пустынь, где преобладает региональный перенос, наряду с углеродом, значительная роль в атмосферных выпадениях холодного времени года принадлежит аммонийным соединениям азота. Суммарное поступление растворимых и нерастворимых форм компонентов в снежный покров снижается при переходе от равнин к горным ... Article in Journal/Newspaper permafrost taiga Tundra Yakutia Якути* Якутия Ice and Snow (E-Journal) Ice and Snow 125 1 73 |