Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago)
Svalbard archipelago is characterized by specific climate conditions, high air temperature and relative air humidity, which are not typical for high latitudes. Such conditions affect soil-forming processes. Classification and morphological structure of the soil cover on the Spitsbergen archipelago a...
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ftmasarykunivojs:oai:ojs.journals.muni.cz:article/12915 2023-05-15T18:29:38+02:00 Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago) Iavid, Elizaveta Iaroslavovna Kondakova, Veronika Nikolaevna Polyakov, Vyacheslav Igorevich Abakumov, Evgeny Vasilyevic 2018-01-01 application/pdf http://journals.muni.cz/CPR/article/view/12915 eng eng Masaryk Univerzity http://journals.muni.cz/CPR/article/view/12915/11267 http://journals.muni.cz/CPR/article/view/12915 Copyright (c) 2020 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0 CC-BY-NC-ND Czech Polar Reports; Vol 8 No 1 (2018); 43-59 Czech Polar Reports; Vol. 8 No. 1 (2018); 43-59 1805-0697 1805-0689 soil Svalbard archipelago Gronfjord area soil diversity soil formation info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2018 ftmasarykunivojs 2022-06-26T10:16:39Z Svalbard archipelago is characterized by specific climate conditions, high air temperature and relative air humidity, which are not typical for high latitudes. Such conditions affect soil-forming processes. Classification and morphological structure of the soil cover on the Spitsbergen archipelago are still poorly understood. The aim of current research was to reveal diverse soil taxons in the Gronfjord area and characterize framework of its formation. As the results of this work, the authors provide the description of the investigated soils and their taxonomy in accordance with World Reference Base for Soil Resources (IUSS Working Group 2015) and the new Russian soil classification system. Chemical parameters of the soil, as well and the data on soil horizons properties were measured using vertical electric resistivity sounding method. In total, 15 soil profiles were made and the studied soils were referred to six Soil Reference Groups with domination of Leptosols and Regosols. The profiles were made in different landscapes that allowed to determine the similarities and differences in soil cover of the area. The main factors affected soil formation are cryogenic processes combined with gleyfication and cambic alteration of soil material. Article in Journal/Newspaper Svalbard Spitsbergen Masaryk University Journals Svalbard Svalbard Archipelago |
institution |
Open Polar |
collection |
Masaryk University Journals |
op_collection_id |
ftmasarykunivojs |
language |
English |
topic |
soil Svalbard archipelago Gronfjord area soil diversity soil formation |
spellingShingle |
soil Svalbard archipelago Gronfjord area soil diversity soil formation Iavid, Elizaveta Iaroslavovna Kondakova, Veronika Nikolaevna Polyakov, Vyacheslav Igorevich Abakumov, Evgeny Vasilyevic Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago) |
topic_facet |
soil Svalbard archipelago Gronfjord area soil diversity soil formation |
description |
Svalbard archipelago is characterized by specific climate conditions, high air temperature and relative air humidity, which are not typical for high latitudes. Such conditions affect soil-forming processes. Classification and morphological structure of the soil cover on the Spitsbergen archipelago are still poorly understood. The aim of current research was to reveal diverse soil taxons in the Gronfjord area and characterize framework of its formation. As the results of this work, the authors provide the description of the investigated soils and their taxonomy in accordance with World Reference Base for Soil Resources (IUSS Working Group 2015) and the new Russian soil classification system. Chemical parameters of the soil, as well and the data on soil horizons properties were measured using vertical electric resistivity sounding method. In total, 15 soil profiles were made and the studied soils were referred to six Soil Reference Groups with domination of Leptosols and Regosols. The profiles were made in different landscapes that allowed to determine the similarities and differences in soil cover of the area. The main factors affected soil formation are cryogenic processes combined with gleyfication and cambic alteration of soil material. |
format |
Article in Journal/Newspaper |
author |
Iavid, Elizaveta Iaroslavovna Kondakova, Veronika Nikolaevna Polyakov, Vyacheslav Igorevich Abakumov, Evgeny Vasilyevic |
author_facet |
Iavid, Elizaveta Iaroslavovna Kondakova, Veronika Nikolaevna Polyakov, Vyacheslav Igorevich Abakumov, Evgeny Vasilyevic |
author_sort |
Iavid, Elizaveta Iaroslavovna |
title |
Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago) |
title_short |
Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago) |
title_full |
Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago) |
title_fullStr |
Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago) |
title_full_unstemmed |
Diversity and main properties of soils of the Gronfjord area (Svalbard archipelago) |
title_sort |
diversity and main properties of soils of the gronfjord area (svalbard archipelago) |
publisher |
Masaryk Univerzity |
publishDate |
2018 |
url |
http://journals.muni.cz/CPR/article/view/12915 |
geographic |
Svalbard Svalbard Archipelago |
geographic_facet |
Svalbard Svalbard Archipelago |
genre |
Svalbard Spitsbergen |
genre_facet |
Svalbard Spitsbergen |
op_source |
Czech Polar Reports; Vol 8 No 1 (2018); 43-59 Czech Polar Reports; Vol. 8 No. 1 (2018); 43-59 1805-0697 1805-0689 |
op_relation |
http://journals.muni.cz/CPR/article/view/12915/11267 http://journals.muni.cz/CPR/article/view/12915 |
op_rights |
Copyright (c) 2020 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0 |
op_rightsnorm |
CC-BY-NC-ND |
_version_ |
1766212817636032512 |