Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ...

The Atacama Desert is the oldest and driest non-polar desert on Earth, where salts have accumulated through atmospheric deposition over millions of years of hyperaridity. These salts can serve as an indicator to provide an understanding of the interaction between water and soil in changing environme...

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Main Authors: Arens, Felix Leo, Airo, Alessandro, Feige, Jenny, Sager, Christof, Wiechert, Uwe, Schulze-Makuch, Dirk
Format: Text
Language:English
Published: Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV) 2023
Subjects:
Online Access:https://dx.doi.org/10.48380/zgaw-zj51
https://www.dggv.de/e-publikationen/salts-as-proxies-for-water-soil-interaction-in-the-hyperarid-atacama-desert
id ftdatacite:10.48380/zgaw-zj51
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spelling ftdatacite:10.48380/zgaw-zj51 2024-01-28T10:08:45+01:00 Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ... Arens, Felix Leo Airo, Alessandro Feige, Jenny Sager, Christof Wiechert, Uwe Schulze-Makuch, Dirk 2023 https://dx.doi.org/10.48380/zgaw-zj51 https://www.dggv.de/e-publikationen/salts-as-proxies-for-water-soil-interaction-in-the-hyperarid-atacama-desert en eng Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV) Abstract ScholaryArticle Text article-journal 2023 ftdatacite https://doi.org/10.48380/zgaw-zj51 2024-01-04T23:34:38Z The Atacama Desert is the oldest and driest non-polar desert on Earth, where salts have accumulated through atmospheric deposition over millions of years of hyperaridity. These salts can serve as an indicator to provide an understanding of the interaction between water and soil in changing environmental conditions. Therefore, four soil profiles were studied for their mineralogy, abundance of salts, and stable isotopic composition of sulfate. In all soil profiles, sulfates are the predominant salts showing a downward transition from gypsum to anhydrite accompanied by an increase in highly soluble salts and a decrease in δ 34 S and δ 18 O values of sulfate. These trends are consistent with downward water infiltration during rare rain events causing salt dissolution and subsequent precipitation in the deeper soil column. This conclusion is also supported by our Rayleigh fractionation model. The presence of anhydrite at >40 cm depth is attributed to their association with nitrate and chloride salts, which ... Text polar desert DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description The Atacama Desert is the oldest and driest non-polar desert on Earth, where salts have accumulated through atmospheric deposition over millions of years of hyperaridity. These salts can serve as an indicator to provide an understanding of the interaction between water and soil in changing environmental conditions. Therefore, four soil profiles were studied for their mineralogy, abundance of salts, and stable isotopic composition of sulfate. In all soil profiles, sulfates are the predominant salts showing a downward transition from gypsum to anhydrite accompanied by an increase in highly soluble salts and a decrease in δ 34 S and δ 18 O values of sulfate. These trends are consistent with downward water infiltration during rare rain events causing salt dissolution and subsequent precipitation in the deeper soil column. This conclusion is also supported by our Rayleigh fractionation model. The presence of anhydrite at >40 cm depth is attributed to their association with nitrate and chloride salts, which ...
format Text
author Arens, Felix Leo
Airo, Alessandro
Feige, Jenny
Sager, Christof
Wiechert, Uwe
Schulze-Makuch, Dirk
spellingShingle Arens, Felix Leo
Airo, Alessandro
Feige, Jenny
Sager, Christof
Wiechert, Uwe
Schulze-Makuch, Dirk
Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ...
author_facet Arens, Felix Leo
Airo, Alessandro
Feige, Jenny
Sager, Christof
Wiechert, Uwe
Schulze-Makuch, Dirk
author_sort Arens, Felix Leo
title Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ...
title_short Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ...
title_full Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ...
title_fullStr Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ...
title_full_unstemmed Salts as proxies for water-soil interaction in the hyperarid Atacama Desert ...
title_sort salts as proxies for water-soil interaction in the hyperarid atacama desert ...
publisher Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV)
publishDate 2023
url https://dx.doi.org/10.48380/zgaw-zj51
https://www.dggv.de/e-publikationen/salts-as-proxies-for-water-soil-interaction-in-the-hyperarid-atacama-desert
genre polar desert
genre_facet polar desert
op_doi https://doi.org/10.48380/zgaw-zj51
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