Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ...

To project the future development of the soil organic carbon (SOC) storage in permafrost environments, the spatial and vertical distribution of key soil properties and their landscape controls needs to be understood. This article reports findings from the Arctic Lena River Delta where we sampled 50...

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Main Authors: Siewert, Matthias Benjamin, Hugelius, Gustaf, Heim, Birgit, Faucherre, Samuel
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2016
Subjects:
Ice
Online Access:https://dx.doi.org/10.1594/pangaea.862961
https://doi.pangaea.de/10.1594/PANGAEA.862961
id ftdatacite:10.1594/pangaea.862961
record_format openpolar
spelling ftdatacite:10.1594/pangaea.862961 2024-09-15T18:11:31+00:00 Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ... Siewert, Matthias Benjamin Hugelius, Gustaf Heim, Birgit Faucherre, Samuel 2016 application/zip https://dx.doi.org/10.1594/pangaea.862961 https://doi.pangaea.de/10.1594/PANGAEA.862961 en eng PANGAEA https://dx.doi.org/10.1016/j.catena.2016.07.048 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Changing Permafrost in the Arctic and its Global Effects in the 21st Century PAGE21 article Collection Supplementary Publication Series of Datasets 2016 ftdatacite https://doi.org/10.1594/pangaea.86296110.1016/j.catena.2016.07.048 2024-07-03T10:38:23Z To project the future development of the soil organic carbon (SOC) storage in permafrost environments, the spatial and vertical distribution of key soil properties and their landscape controls needs to be understood. This article reports findings from the Arctic Lena River Delta where we sampled 50 soil pedons. These were classified according to the U.S.D.A. Soil Taxonomy and fall mostly into the Gelisol soil order used for permafrost-affected soils. Soil profiles have been sampled for the active layer (mean depth 58 ± 10 cm) and the upper permafrost to one meter depth. We analyze SOC stocks and key soil properties, i.e. C%, N%, C/N, bulk density, visible ice and water content. These are compared for different landscape groupings of pedons according to geomorphology, soil and land cover and for different vertical depth increments. High vertical resolution plots are used to understand soil development. These show that SOC storage can be highly variable with depth. We recommend the treatment of ... : Supplement to: Siewert, Matthias Benjamin; Hugelius, Gustaf; Heim, Birgit; Faucherre, Samuel (2016): Landscape controls and vertical variability of soil organic carbon storage in permafrost-affected soils of the Lena River Delta. CATENA, 147, 725-741 ... Article in Journal/Newspaper Ice lena river permafrost DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Changing Permafrost in the Arctic and its Global Effects in the 21st Century PAGE21
spellingShingle Changing Permafrost in the Arctic and its Global Effects in the 21st Century PAGE21
Siewert, Matthias Benjamin
Hugelius, Gustaf
Heim, Birgit
Faucherre, Samuel
Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ...
topic_facet Changing Permafrost in the Arctic and its Global Effects in the 21st Century PAGE21
description To project the future development of the soil organic carbon (SOC) storage in permafrost environments, the spatial and vertical distribution of key soil properties and their landscape controls needs to be understood. This article reports findings from the Arctic Lena River Delta where we sampled 50 soil pedons. These were classified according to the U.S.D.A. Soil Taxonomy and fall mostly into the Gelisol soil order used for permafrost-affected soils. Soil profiles have been sampled for the active layer (mean depth 58 ± 10 cm) and the upper permafrost to one meter depth. We analyze SOC stocks and key soil properties, i.e. C%, N%, C/N, bulk density, visible ice and water content. These are compared for different landscape groupings of pedons according to geomorphology, soil and land cover and for different vertical depth increments. High vertical resolution plots are used to understand soil development. These show that SOC storage can be highly variable with depth. We recommend the treatment of ... : Supplement to: Siewert, Matthias Benjamin; Hugelius, Gustaf; Heim, Birgit; Faucherre, Samuel (2016): Landscape controls and vertical variability of soil organic carbon storage in permafrost-affected soils of the Lena River Delta. CATENA, 147, 725-741 ...
format Article in Journal/Newspaper
author Siewert, Matthias Benjamin
Hugelius, Gustaf
Heim, Birgit
Faucherre, Samuel
author_facet Siewert, Matthias Benjamin
Hugelius, Gustaf
Heim, Birgit
Faucherre, Samuel
author_sort Siewert, Matthias Benjamin
title Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ...
title_short Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ...
title_full Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ...
title_fullStr Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ...
title_full_unstemmed Soil organic carbon storage and soil properties for 50 soil profiles in the Lena River Delta including land form description and map ...
title_sort soil organic carbon storage and soil properties for 50 soil profiles in the lena river delta including land form description and map ...
publisher PANGAEA
publishDate 2016
url https://dx.doi.org/10.1594/pangaea.862961
https://doi.pangaea.de/10.1594/PANGAEA.862961
genre Ice
lena river
permafrost
genre_facet Ice
lena river
permafrost
op_relation https://dx.doi.org/10.1016/j.catena.2016.07.048
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.86296110.1016/j.catena.2016.07.048
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