Pan-Arctic soil element availability estimations ...

Arctic soils store large amounts of organic carbon and other elements. Here, we analyzed amorphous silica (ASi), silicon (Si), calcium (Ca), iron (Fe), phosphorus (P), and aluminum (Al) availability from 574 soil samples from around the Arctic region. We summarized these data in pan-Arctic maps of A...

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Main Authors: Schaller, Jörg, Göckede, Mathias
Format: Dataset
Language:unknown
Published: Edmond 2023
Subjects:
Online Access:https://dx.doi.org/10.17617/3.8kgqun
https://edmond.mpdl.mpg.de/citation?persistentId=doi:10.17617/3.8KGQUN
id ftdatacite:10.17617/3.8kgqun
record_format openpolar
spelling ftdatacite:10.17617/3.8kgqun 2023-05-15T14:32:40+02:00 Pan-Arctic soil element availability estimations ... Schaller, Jörg Göckede, Mathias 2023 https://dx.doi.org/10.17617/3.8kgqun https://edmond.mpdl.mpg.de/citation?persistentId=doi:10.17617/3.8KGQUN unknown Edmond dataset Dataset 2023 ftdatacite https://doi.org/10.17617/3.8kgqun 2023-04-03T17:39:58Z Arctic soils store large amounts of organic carbon and other elements. Here, we analyzed amorphous silica (ASi), silicon (Si), calcium (Ca), iron (Fe), phosphorus (P), and aluminum (Al) availability from 574 soil samples from around the Arctic region. We summarized these data in pan-Arctic maps of ASi, Si, Ca, Fe, P, and Al concentrations focusing on the top 100 cm of Arctic soil. Furthermore, we provide values for element availability for the organic and the mineral layer of the seasonally thawing active layer as well as for the uppermost permafrost layer. We show large differences in ASi, Si, Ca, Fe, P, and Al availability between different lithologies and Arctic regions. Our provided spatially explicit data on differences in the availability of elements between the different lithological classes and regions now and in the future will improve Arctic models for estimating current and future carbon and nutrient feedbacks under climate change. ... Dataset Arctic Climate change permafrost DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description Arctic soils store large amounts of organic carbon and other elements. Here, we analyzed amorphous silica (ASi), silicon (Si), calcium (Ca), iron (Fe), phosphorus (P), and aluminum (Al) availability from 574 soil samples from around the Arctic region. We summarized these data in pan-Arctic maps of ASi, Si, Ca, Fe, P, and Al concentrations focusing on the top 100 cm of Arctic soil. Furthermore, we provide values for element availability for the organic and the mineral layer of the seasonally thawing active layer as well as for the uppermost permafrost layer. We show large differences in ASi, Si, Ca, Fe, P, and Al availability between different lithologies and Arctic regions. Our provided spatially explicit data on differences in the availability of elements between the different lithological classes and regions now and in the future will improve Arctic models for estimating current and future carbon and nutrient feedbacks under climate change. ...
format Dataset
author Schaller, Jörg
Göckede, Mathias
spellingShingle Schaller, Jörg
Göckede, Mathias
Pan-Arctic soil element availability estimations ...
author_facet Schaller, Jörg
Göckede, Mathias
author_sort Schaller, Jörg
title Pan-Arctic soil element availability estimations ...
title_short Pan-Arctic soil element availability estimations ...
title_full Pan-Arctic soil element availability estimations ...
title_fullStr Pan-Arctic soil element availability estimations ...
title_full_unstemmed Pan-Arctic soil element availability estimations ...
title_sort pan-arctic soil element availability estimations ...
publisher Edmond
publishDate 2023
url https://dx.doi.org/10.17617/3.8kgqun
https://edmond.mpdl.mpg.de/citation?persistentId=doi:10.17617/3.8KGQUN
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
permafrost
genre_facet Arctic
Climate change
permafrost
op_doi https://doi.org/10.17617/3.8kgqun
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