The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ...
Dissolved organic matter (DOM) in glacier environments is aliphatic-rich, yet studies have proposed DOM originates from allochthonous, aromatic and often aged material. Allochthonous organic matter (OM) is exposed to ultraviolet radiation both in atmospheric transport and post-deposition on the glac...
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Interdisciplinary Earth Data Alliance (IEDA)
2021
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Online Access: | https://dx.doi.org/10.26022/ieda/111996 https://ecl.earthchem.org/view.php?id=1996 |
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ftdatacite:10.26022/ieda/111996 2024-02-27T08:40:44+00:00 The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ... Holt, Amy Kellerman, Anne Stubbins , Aron Wagner, Sasha McKenna, Amy Fellman, Jason Hood, Eran Spencer, Robert 2021 application/vnd.ms-excel https://dx.doi.org/10.26022/ieda/111996 https://ecl.earthchem.org/view.php?id=1996 en eng Interdisciplinary Earth Data Alliance (IEDA) Creative Commons Attribution Share Alike 4.0 International https://creativecommons.org/licenses/by-sa/4.0/legalcode cc-by-sa-4.0 Other dissolved organic matter, glaciers, water soluble organic carbon, atmospheric deposition, FT-ICR MS dataset Dataset 2021 ftdatacite https://doi.org/10.26022/ieda/111996 2024-02-01T15:06:42Z Dissolved organic matter (DOM) in glacier environments is aliphatic-rich, yet studies have proposed DOM originates from allochthonous, aromatic and often aged material. Allochthonous organic matter (OM) is exposed to ultraviolet radiation both in atmospheric transport and post-deposition on the glacier surface. Thus, we evaluate photochemistry as a mechanism to account for the compositional disconnect between allochthonous OM sources and glacier DOM composition. Six solid endmember OM sources were leached in ultrapure water and photo-irradiated for 28-days in a solar simulator, until > 90 % of initial chromophoric DOM was removed. Ultrahigh-resolution mass spectrometry was used to compare the molecular composition of leachates pre- and post-irradiation to DOM sampled from supraglacial and bulk runoff from the Greenland Ice Sheet and Juneau Icefield, respectively. Photo-irradiation drove molecular level convergence between the initially aromatic-rich leachates and aromatic-poor glacial samples, selectively ... Dataset glacier Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland Juneau Icefield ENVELOPE(-134.254,-134.254,58.916,58.916) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Other dissolved organic matter, glaciers, water soluble organic carbon, atmospheric deposition, FT-ICR MS |
spellingShingle |
Other dissolved organic matter, glaciers, water soluble organic carbon, atmospheric deposition, FT-ICR MS Holt, Amy Kellerman, Anne Stubbins , Aron Wagner, Sasha McKenna, Amy Fellman, Jason Hood, Eran Spencer, Robert The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ... |
topic_facet |
Other dissolved organic matter, glaciers, water soluble organic carbon, atmospheric deposition, FT-ICR MS |
description |
Dissolved organic matter (DOM) in glacier environments is aliphatic-rich, yet studies have proposed DOM originates from allochthonous, aromatic and often aged material. Allochthonous organic matter (OM) is exposed to ultraviolet radiation both in atmospheric transport and post-deposition on the glacier surface. Thus, we evaluate photochemistry as a mechanism to account for the compositional disconnect between allochthonous OM sources and glacier DOM composition. Six solid endmember OM sources were leached in ultrapure water and photo-irradiated for 28-days in a solar simulator, until > 90 % of initial chromophoric DOM was removed. Ultrahigh-resolution mass spectrometry was used to compare the molecular composition of leachates pre- and post-irradiation to DOM sampled from supraglacial and bulk runoff from the Greenland Ice Sheet and Juneau Icefield, respectively. Photo-irradiation drove molecular level convergence between the initially aromatic-rich leachates and aromatic-poor glacial samples, selectively ... |
format |
Dataset |
author |
Holt, Amy Kellerman, Anne Stubbins , Aron Wagner, Sasha McKenna, Amy Fellman, Jason Hood, Eran Spencer, Robert |
author_facet |
Holt, Amy Kellerman, Anne Stubbins , Aron Wagner, Sasha McKenna, Amy Fellman, Jason Hood, Eran Spencer, Robert |
author_sort |
Holt, Amy |
title |
The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ... |
title_short |
The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ... |
title_full |
The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ... |
title_fullStr |
The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ... |
title_full_unstemmed |
The Role of Photochemistry in Driving the Composition of Dissolved Organic Matter Found in Glacier Environments ... |
title_sort |
role of photochemistry in driving the composition of dissolved organic matter found in glacier environments ... |
publisher |
Interdisciplinary Earth Data Alliance (IEDA) |
publishDate |
2021 |
url |
https://dx.doi.org/10.26022/ieda/111996 https://ecl.earthchem.org/view.php?id=1996 |
long_lat |
ENVELOPE(-134.254,-134.254,58.916,58.916) |
geographic |
Greenland Juneau Icefield |
geographic_facet |
Greenland Juneau Icefield |
genre |
glacier Greenland Ice Sheet |
genre_facet |
glacier Greenland Ice Sheet |
op_rights |
Creative Commons Attribution Share Alike 4.0 International https://creativecommons.org/licenses/by-sa/4.0/legalcode cc-by-sa-4.0 |
op_doi |
https://doi.org/10.26022/ieda/111996 |
_version_ |
1792047868201140224 |