Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens
International audience The variation of B concentration in atmospheric deposition was studied fromanalysis of 35 individual rain events, 17 snow packs, and 17 lichens sampled over NE North America (south from Hudson Bay) and Asia (from the coast of Bangladesh to the high Himalayas of Nepal). Rain sa...
Published in: | Geochemistry, Geophysics, Geosystems |
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Language: | English |
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ftunilorrainehal:oai:HAL:insu-01882122v1 2023-10-09T21:52:13+02:00 Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens Rose, E, F Carignan, J. Chaussidon, M. Centre de Recherches Pétrographiques et Géochimiques (CRPG) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS) Woods Hole Oceanographic Institution (WHOI) 2000-11-10 https://insu.hal.science/insu-01882122 https://insu.hal.science/insu-01882122/document https://insu.hal.science/insu-01882122/file/Rose_et_al-2000-Geochemistry%252C_Geophysics%252C_Geosystems.pdf https://doi.org/10.1029/2000GC000077 en eng HAL CCSD AGU and the Geochemical Society info:eu-repo/semantics/altIdentifier/doi/10.1029/2000GC000077 insu-01882122 https://insu.hal.science/insu-01882122 https://insu.hal.science/insu-01882122/document https://insu.hal.science/insu-01882122/file/Rose_et_al-2000-Geochemistry%252C_Geophysics%252C_Geosystems.pdf doi:10.1029/2000GC000077 info:eu-repo/semantics/OpenAccess ISSN: 1525-2027 EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://insu.hal.science/insu-01882122 Geochemistry, Geophysics, Geosystems, 2000, 1 (11), ⟨10.1029/2000GC000077⟩ rains Boron concentration atmosphere lichens aerosols [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.OCEAN]Sciences of the Universe [physics]/Ocean info:eu-repo/semantics/article Journal articles 2000 ftunilorrainehal https://doi.org/10.1029/2000GC000077 2023-09-12T23:19:04Z International audience The variation of B concentration in atmospheric deposition was studied fromanalysis of 35 individual rain events, 17 snow packs, and 17 lichens sampled over NE North America (south from Hudson Bay) and Asia (from the coast of Bangladesh to the high Himalayas of Nepal). Rain samples show a range of B concentration between 0.3 and 9.4 μg/L (average of 1.8 ± 1.7 μg/L), excluding two rains with higher B contents of 17 and 37.5 μg/L, most likely reflecting anthropic contamination. Snowpacks and lichens which average atmospheric deposition over periods of a few months to a few years show a smaller range of variation, from 0.1 to 2.3 μg/L (average 1.1 ± 0.8 μg/L) for snowpacks and from 1 to 25.9 ppm for lichens. The lichens have elemental ratios (such as B/Cl) similar to the average of rains, showing that they are good monitors of atmospheric B deposition without significant biofractionation of elements. This is also demonstrated by their halogen contents, which follow the systematics of the atmospheric distribution of these elements previously derived from the study of rains and atmospheric particles. Though individual rains do not show systematic decrease in B concentration with distance to the sea, this behavior is clearly shown by samples having longer integration times, snowpacks, and lichens. The snow and lichen data show that seawater is a major source of atmospheric B. Using the lichen data, the enrichment factor (normalized to Na) of marine air masses relative to seawater is estimated to be ∼13 (average B/Na of 5.6 × 10−3). This implies that the fractionation factor of atmospheric suspended marine particles relative to seawater (FX = (X/Na)particle/(X/Na)seawater) is 0.177. Thus B transfer from seawater to the atmosphere occurs mostly via degassing of sea salts, the residence time of gaseous B being estimated at 15.9‐fold that of particulate B. The distribution of B in the atmosphere between gaseous B and degassed sea salts can be used to model the large range of B concentrations ... Article in Journal/Newspaper Hudson Bay Université de Lorraine: HAL Hudson Hudson Bay Geochemistry, Geophysics, Geosystems 1 11 n/a n/a |
institution |
Open Polar |
collection |
Université de Lorraine: HAL |
op_collection_id |
ftunilorrainehal |
language |
English |
topic |
rains Boron concentration atmosphere lichens aerosols [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.OCEAN]Sciences of the Universe [physics]/Ocean |
spellingShingle |
rains Boron concentration atmosphere lichens aerosols [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Rose, E, F Carignan, J. Chaussidon, M. Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens |
topic_facet |
rains Boron concentration atmosphere lichens aerosols [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.OCEAN]Sciences of the Universe [physics]/Ocean |
description |
International audience The variation of B concentration in atmospheric deposition was studied fromanalysis of 35 individual rain events, 17 snow packs, and 17 lichens sampled over NE North America (south from Hudson Bay) and Asia (from the coast of Bangladesh to the high Himalayas of Nepal). Rain samples show a range of B concentration between 0.3 and 9.4 μg/L (average of 1.8 ± 1.7 μg/L), excluding two rains with higher B contents of 17 and 37.5 μg/L, most likely reflecting anthropic contamination. Snowpacks and lichens which average atmospheric deposition over periods of a few months to a few years show a smaller range of variation, from 0.1 to 2.3 μg/L (average 1.1 ± 0.8 μg/L) for snowpacks and from 1 to 25.9 ppm for lichens. The lichens have elemental ratios (such as B/Cl) similar to the average of rains, showing that they are good monitors of atmospheric B deposition without significant biofractionation of elements. This is also demonstrated by their halogen contents, which follow the systematics of the atmospheric distribution of these elements previously derived from the study of rains and atmospheric particles. Though individual rains do not show systematic decrease in B concentration with distance to the sea, this behavior is clearly shown by samples having longer integration times, snowpacks, and lichens. The snow and lichen data show that seawater is a major source of atmospheric B. Using the lichen data, the enrichment factor (normalized to Na) of marine air masses relative to seawater is estimated to be ∼13 (average B/Na of 5.6 × 10−3). This implies that the fractionation factor of atmospheric suspended marine particles relative to seawater (FX = (X/Na)particle/(X/Na)seawater) is 0.177. Thus B transfer from seawater to the atmosphere occurs mostly via degassing of sea salts, the residence time of gaseous B being estimated at 15.9‐fold that of particulate B. The distribution of B in the atmosphere between gaseous B and degassed sea salts can be used to model the large range of B concentrations ... |
author2 |
Centre de Recherches Pétrographiques et Géochimiques (CRPG) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS) Woods Hole Oceanographic Institution (WHOI) |
format |
Article in Journal/Newspaper |
author |
Rose, E, F Carignan, J. Chaussidon, M. |
author_facet |
Rose, E, F Carignan, J. Chaussidon, M. |
author_sort |
Rose, E, F |
title |
Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens |
title_short |
Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens |
title_full |
Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens |
title_fullStr |
Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens |
title_full_unstemmed |
Transfer of atmospheric boron from the oceans to the continents: An investigation using precipitation waters and epiphytic lichens |
title_sort |
transfer of atmospheric boron from the oceans to the continents: an investigation using precipitation waters and epiphytic lichens |
publisher |
HAL CCSD |
publishDate |
2000 |
url |
https://insu.hal.science/insu-01882122 https://insu.hal.science/insu-01882122/document https://insu.hal.science/insu-01882122/file/Rose_et_al-2000-Geochemistry%252C_Geophysics%252C_Geosystems.pdf https://doi.org/10.1029/2000GC000077 |
geographic |
Hudson Hudson Bay |
geographic_facet |
Hudson Hudson Bay |
genre |
Hudson Bay |
genre_facet |
Hudson Bay |
op_source |
ISSN: 1525-2027 EISSN: 1525-2027 Geochemistry, Geophysics, Geosystems https://insu.hal.science/insu-01882122 Geochemistry, Geophysics, Geosystems, 2000, 1 (11), ⟨10.1029/2000GC000077⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2000GC000077 insu-01882122 https://insu.hal.science/insu-01882122 https://insu.hal.science/insu-01882122/document https://insu.hal.science/insu-01882122/file/Rose_et_al-2000-Geochemistry%252C_Geophysics%252C_Geosystems.pdf doi:10.1029/2000GC000077 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2000GC000077 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
1 |
container_issue |
11 |
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