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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10296
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dc.contributor.authorallBobrowski, N.; Institut für Umweltphysik, University of Heidelberg, Heidelberg, Germanyen
dc.contributor.authorallvon Glasow, R.; 2Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, United Kingdomen
dc.contributor.authorallGiuffrida, G. B.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallTedesco, D.; Department of Environmental Sciences, Second University of Napoli, Caserta, Italyen
dc.contributor.authorallAiuppa, A.; Dipartimento Scienze della Terra e del Mare, University of Palermo, Palermo, Italy,en
dc.contributor.authorallYalire, M.; Observatoire Volcanologique de Goma, Goma, Democratic Republic of Congoen
dc.contributor.authorallArellano, S.; Department of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Swedenen
dc.contributor.authorallJohansson, M.; Department of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Swedenen
dc.contributor.authorallGalle, B.; Department of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Swedenen
dc.date.accessioned2016-04-13T12:52:38Zen
dc.date.available2016-04-13T12:52:38Zen
dc.date.issued2015-01-12en
dc.identifier.urihttp://hdl.handle.net/2122/10296en
dc.description.abstractAirborne and ground-based differential optical absorption spectroscopy observations have been carried out at the volcano Nyiragongo (Democratic Republic of Congo) tomeasure SO2 and bromine monoxide (BrO) in the plume inMarch 2004 and June 2007, respectively. Additionally filter pack andmulticomponent gas analyzer system (Multi-GAS)measurements were carried out in June 2007. Ourmeasurements provide valuable information on the chemical composition of the volcanic plume emitted fromthe lava lake of Nyiragongo. The main interest of this study has been to investigate for the first time the bromine emission flux of Nyiragongo (a rift volcano) and the BrO formation in its volcanic plume. Measurement data and results from a numerical model of the evolution of BrO in Nyiragongo volcanic plume are compared with earlier studies of the volcanic plume of Etna (Italy). Even though the bromine flux from Nyiragongo (2.6 t/d) is slightly greater than that from Etna (1.9 t/d), the BrO/SO2 ratio (maximum 7 × 10 5) is smaller than in the plume of Etna (maximum 2.1 × 10 4). A one-dimensional photochemical model to investigate halogen chemistry in the volcanic plumes of Etna and Nyiragongo was initialized using data from Multi-GAS and filter pack measurements. Model runs showed that the differences in the composition of volcanic volatiles led to a smaller fraction of total bromine being present as BrO in the Nyiragongo plume and to a smaller BrO/SO2 ratio.en
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofJournal of geophysical research - atmospheresen
dc.relation.ispartofseries/120(2015)en
dc.subjectIntraplate volcano Nyiragongo is bromine rich although chlorine pooren
dc.subjectBrO/Br in volcanic plumes depends on initial plume compositionen
dc.subjectDetermination of Nyiragongo chlorine, bromine, sulfur emission strengthen
dc.titleGas emission strength and evolution of the molar ratio of BrO/SO2 in the plume of Nyiragongo in comparison to Etnaen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber277-291en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.01. Gasesen
dc.identifier.doi10.1002/2013JD021069en
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dc.description.obiettivoSpecifico4V. Vulcani e ambienteen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0148-0227en
dc.contributor.authorBobrowski, N.en
dc.contributor.authorvon Glasow, R.en
dc.contributor.authorGiuffrida, G. B.en
dc.contributor.authorTedesco, D.en
dc.contributor.authorAiuppa, A.en
dc.contributor.authorYalire, M.en
dc.contributor.authorArellano, S.en
dc.contributor.authorJohansson, M.en
dc.contributor.authorGalle, B.en
dc.contributor.departmentInstitut für Umweltphysik, University of Heidelberg, Heidelberg, Germanyen
dc.contributor.department2Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, United Kingdomen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentDepartment of Environmental Sciences, Second University of Napoli, Caserta, Italyen
dc.contributor.departmentDipartimento Scienze della Terra e del Mare, University of Palermo, Palermo, Italy,en
dc.contributor.departmentObservatoire Volcanologique de Goma, Goma, Democratic Republic of Congoen
dc.contributor.departmentDepartment of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Swedenen
dc.contributor.departmentDepartment of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Swedenen
dc.contributor.departmentDepartment of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Swedenen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptSchool of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptChalmers University of Technology, Horsalsvagen 11, SE-412 96 Gothenburg, Sweden-
crisitem.author.orcid0000-0003-3072-4088-
crisitem.author.orcid0000-0002-0254-6539-
crisitem.author.orcid0000-0002-0306-3782-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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