The sulfur budget of the 2011 Grímsvötn eruption, Iceland
International audience Sulfur concentrations have been measured in 28 melt inclusions (MIs) in plagioclase, clinopyroxene, and olivine crystals extracted from tephra produced during the explosive eruption of Grímsvötn in May 2011. The results are compared to sulfur concentrations in the groundmass g...
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Online Access: | https://hal.science/hal-00992831 https://hal.science/hal-00992831/document https://hal.science/hal-00992831/file/Geophysical%20Research%20Letters%20-%202013%20-%20Sigmarsson%20-%20The%20sulfur%20budget%20of%20the%202011%20Gr%20msv%20tn%20eruption%20Iceland.pdf https://doi.org/10.1002/2013GL057760 |
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ftinsu:oai:HAL:hal-00992831v1 2024-02-04T10:01:30+01:00 The sulfur budget of the 2011 Grímsvötn eruption, Iceland Sigmarsson, Olgeir Haddadi, Baptiste Carn, Simon Moune, Séverine Gudnason, Jonas Yang, Kai Clarisse, Lieven Laboratoire Magmas et Volcans (LMV) Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS) Institute of Earth Sciences Reykjavik University of Iceland Reykjavik Department of Geological and Mining Engineering and Sciences Michigan Technological University (MTU) Atmospheric Chemistry and Dynamics Laboratory Greenbelt NASA Goddard Space Flight Center (GSFC) Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique Université libre de Bruxelles (ULB) 2013 https://hal.science/hal-00992831 https://hal.science/hal-00992831/document https://hal.science/hal-00992831/file/Geophysical%20Research%20Letters%20-%202013%20-%20Sigmarsson%20-%20The%20sulfur%20budget%20of%20the%202011%20Gr%20msv%20tn%20eruption%20Iceland.pdf https://doi.org/10.1002/2013GL057760 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2013GL057760 hal-00992831 https://hal.science/hal-00992831 https://hal.science/hal-00992831/document https://hal.science/hal-00992831/file/Geophysical%20Research%20Letters%20-%202013%20-%20Sigmarsson%20-%20The%20sulfur%20budget%20of%20the%202011%20Gr%20msv%20tn%20eruption%20Iceland.pdf doi:10.1002/2013GL057760 http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-00992831 Geophysical Research Letters, 2013, 40, pp.6095-6100. ⟨10.1002/2013GL057760⟩ sulfur degassing Grímsvötn volcano satellite-based SO2 mass loading sulfide globules mineral melt inclusions [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2013 ftinsu https://doi.org/10.1002/2013GL057760 2024-01-10T17:25:16Z International audience Sulfur concentrations have been measured in 28 melt inclusions (MIs) in plagioclase, clinopyroxene, and olivine crystals extracted from tephra produced during the explosive eruption of Grímsvötn in May 2011. The results are compared to sulfur concentrations in the groundmass glass in order to estimate the mass of sulfur brought to surface during the eruption. Satellite measurements yield order of magnitude lower sulfur (~0.2 Tg) in the eruption plume than estimated from the difference between MI and the groundmass glass. This sulfur "deficit" is readily explained by sulfur adhering to tephra grains but principally by sulfide globules caused by basalt-sulfide melt exsolution before degassing. A mass balance calculation reveals that approximately ~0.8 Tg of SO2 is present as globules, representing ~50% of the total sulfur budget. Most of the sulfide globules likely reside at depth due to their elevated density, for potential later remobilization by new magma or hydrothermal circulation. Article in Journal/Newspaper Iceland Institut national des sciences de l'Univers: HAL-INSU Geophysical Research Letters 40 23 6095 6100 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
sulfur degassing Grímsvötn volcano satellite-based SO2 mass loading sulfide globules mineral melt inclusions [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
sulfur degassing Grímsvötn volcano satellite-based SO2 mass loading sulfide globules mineral melt inclusions [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes Sigmarsson, Olgeir Haddadi, Baptiste Carn, Simon Moune, Séverine Gudnason, Jonas Yang, Kai Clarisse, Lieven The sulfur budget of the 2011 Grímsvötn eruption, Iceland |
topic_facet |
sulfur degassing Grímsvötn volcano satellite-based SO2 mass loading sulfide globules mineral melt inclusions [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience Sulfur concentrations have been measured in 28 melt inclusions (MIs) in plagioclase, clinopyroxene, and olivine crystals extracted from tephra produced during the explosive eruption of Grímsvötn in May 2011. The results are compared to sulfur concentrations in the groundmass glass in order to estimate the mass of sulfur brought to surface during the eruption. Satellite measurements yield order of magnitude lower sulfur (~0.2 Tg) in the eruption plume than estimated from the difference between MI and the groundmass glass. This sulfur "deficit" is readily explained by sulfur adhering to tephra grains but principally by sulfide globules caused by basalt-sulfide melt exsolution before degassing. A mass balance calculation reveals that approximately ~0.8 Tg of SO2 is present as globules, representing ~50% of the total sulfur budget. Most of the sulfide globules likely reside at depth due to their elevated density, for potential later remobilization by new magma or hydrothermal circulation. |
author2 |
Laboratoire Magmas et Volcans (LMV) Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS) Institute of Earth Sciences Reykjavik University of Iceland Reykjavik Department of Geological and Mining Engineering and Sciences Michigan Technological University (MTU) Atmospheric Chemistry and Dynamics Laboratory Greenbelt NASA Goddard Space Flight Center (GSFC) Spectroscopie de l'atmosphère, Service de Chimie Quantique et Photophysique Université libre de Bruxelles (ULB) |
format |
Article in Journal/Newspaper |
author |
Sigmarsson, Olgeir Haddadi, Baptiste Carn, Simon Moune, Séverine Gudnason, Jonas Yang, Kai Clarisse, Lieven |
author_facet |
Sigmarsson, Olgeir Haddadi, Baptiste Carn, Simon Moune, Séverine Gudnason, Jonas Yang, Kai Clarisse, Lieven |
author_sort |
Sigmarsson, Olgeir |
title |
The sulfur budget of the 2011 Grímsvötn eruption, Iceland |
title_short |
The sulfur budget of the 2011 Grímsvötn eruption, Iceland |
title_full |
The sulfur budget of the 2011 Grímsvötn eruption, Iceland |
title_fullStr |
The sulfur budget of the 2011 Grímsvötn eruption, Iceland |
title_full_unstemmed |
The sulfur budget of the 2011 Grímsvötn eruption, Iceland |
title_sort |
sulfur budget of the 2011 grímsvötn eruption, iceland |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal.science/hal-00992831 https://hal.science/hal-00992831/document https://hal.science/hal-00992831/file/Geophysical%20Research%20Letters%20-%202013%20-%20Sigmarsson%20-%20The%20sulfur%20budget%20of%20the%202011%20Gr%20msv%20tn%20eruption%20Iceland.pdf https://doi.org/10.1002/2013GL057760 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-00992831 Geophysical Research Letters, 2013, 40, pp.6095-6100. ⟨10.1002/2013GL057760⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/2013GL057760 hal-00992831 https://hal.science/hal-00992831 https://hal.science/hal-00992831/document https://hal.science/hal-00992831/file/Geophysical%20Research%20Letters%20-%202013%20-%20Sigmarsson%20-%20The%20sulfur%20budget%20of%20the%202011%20Gr%20msv%20tn%20eruption%20Iceland.pdf doi:10.1002/2013GL057760 |
op_rights |
http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1002/2013GL057760 |
container_title |
Geophysical Research Letters |
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40 |
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23 |
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