Post-depositional loss of nitrate and chloride in Antarctic snow by photolysis and sublimation: a field investigation
Nitrate in snow is subject to post-depositional processing, which leads to a net loss and redistribution within the snowpack. The relative importance of post-depositional loss processes such as the volatilization of nitric acid (HNO3) and photolysis of nitrate has long been debated. Changes in nitra...
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| Published in | Polar research Vol. 39; pp. 1 - 9 |
|---|---|
| Main Authors | , |
| Format | Journal Article |
| Language | English |
| Published |
Spånga
Open Academia
28.12.2020
Norwegian Polar Institute |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0800-0395 1751-8369 1751-8369 |
| DOI | 10.33265/polar.v39.5146 |
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| Abstract | Nitrate in snow is subject to post-depositional processing, which leads to a net loss and redistribution within the snowpack. The relative importance of post-depositional loss processes such as the volatilization of nitric acid (HNO3) and photolysis of nitrate has long been debated. Changes in nitrate and chloride concentrations in the snowpack were investigated at H128 (69°23.584’S, 41°33.712’E), an Antarctic coastal site approximately 100 km from Syowa Station in East Antarctica from December 2015 to February 2016. Results indicate that chloride migrated to deeper sites within the snowpack under the influence of water vapour movement. Moreover, 50% of the nitrate on surface snow was lost to photolysis, and approximately 20% of the nitrate was absent at a depth of 40 cm. To enhance our knowledge of the Antarctic geochemical cycle, this study is the first to suggest chloride ion movement in snowpacks or significant nitrate loss for any Antarctic coastal site. |
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| AbstractList | Nitrate in snow is subject to post-depositional processing, which leads to a net loss and redistribution within the snowpack. The relative importance of post-depositional loss processes such as the volatilization of nitric acid (HNO3) and photolysis of nitrate has long been debated. Changes in nitrate and chloride concentrations in the snowpack were investigated at H128 (69°23.584’S, 41°33.712’E), an Antarctic coastal site approximately 100 km from Syowa Station in East Antarctica from December 2015 to February 2016. Results indicate that chloride migrated to deeper sites within the snowpack under the influence of water vapour movement. Moreover, 50% of the nitrate on surface snow was lost to photolysis, and approximately 20% of the nitrate was absent at a depth of 40 cm. To enhance our knowledge of the Antarctic geochemical cycle, this study is the first to suggest chloride ion movement in snowpacks or significant nitrate loss for any Antarctic coastal site. |
| Author | Takenaka, Norimichi Noro, Kazushi |
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| CitedBy_id | crossref_primary_10_1016_j_marpolbul_2021_112561 crossref_primary_10_1038_s41467_022_31855_7 crossref_primary_10_1029_2021JD035062 |
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| SubjectTerms | antarctica Chloride ions Chlorides Chromatography Field investigations Geochemical cycle Geochemical cycles Homogenization Hydrochloric acid Ice Laboratories Net losses Nitrates Nitric acid Nitric acids nitrogen cycle nitrogen oxides ozone Photolysis Snow Snowpack Soil sciences Sublimation Volatilization Water vapor Water vapour |
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| Title | Post-depositional loss of nitrate and chloride in Antarctic snow by photolysis and sublimation: a field investigation |
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