Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5101
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dc.contributor.authorallVon Glasow, R.; School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UKen
dc.contributor.authorallBobrowski, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallKern, C.; Institut für Umweltphysik, Universität Heidelberg, Im Neuenheimer Feld 229, 69120 Heidelberg, Germanyen
dc.date.accessioned2009-06-25T13:11:27Zen
dc.date.available2009-06-25T13:11:27Zen
dc.date.issued2009-06-15en
dc.identifier.urihttp://hdl.handle.net/2122/5101en
dc.description.abstractVolcanoes are very strong sources of sulphur, acids and other gases, as well as particles, that are of atmospheric relevance. Some gases only behave as passive tracers, others affect the formation, growth or chemical characteristics of aerosol particles and many lead to adverse effects on vegetation and human health when deposited in the vicinity of volcanoes. In this article the main effects of volcanic emissions on atmospheric chemistry are discussed, with a focus on sulphur and halogen compounds, and to a smaller extent on climate. We primarily focus on quiescent degassing but the main effects of explosive eruptions on the troposphere and stratosphere are covered as well. The key distinction between chemistry in magmatic and hydrothermal settings and the atmosphere is that the atmosphere is oxidising whereas the chemistry is typically reducing in the former cases due to very low oxygen concentrations. Rapid catalytic cycles involving radicals are a further characteristic of atmospheric chemistry. Most reaction cycles involve the photolysis of molecules as a key part of the reaction chains. Recent measurements of halogen radicals in volcanic plumes showed that volcanic plumes are chemically very active. We explain the formation mechanism of halogen oxides in plumes as well as their relevance for the atmosphere.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofChemical Geologyen
dc.relation.ispartofseries1-4/263(2009)en
dc.subjectQuiescent degassingen
dc.subjectTroposphereen
dc.subjectHalogensen
dc.subjectAtmospheric chemistryen
dc.titleThe effects of volcanic eruptions on atmospheric chemistryen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber131-142en
dc.identifier.URLhttp://scienceserver.cilea.it/pdflinks/09052514071407948.pdfen
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.07. Volcanic effectsen
dc.identifier.doi10.1016/j.chemgeo.2008.08.020en
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dc.description.obiettivoSpecifico1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attiveen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorVon Glasow, R.en
dc.contributor.authorBobrowski, N.en
dc.contributor.authorKern, C.en
dc.contributor.departmentSchool of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UKen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentInstitut für Umweltphysik, Universität Heidelberg, Im Neuenheimer Feld 229, 69120 Heidelberg, Germanyen
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item.fulltextWith Fulltext-
crisitem.author.deptSchool of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK-
crisitem.author.deptU.S. Geological Survey, Cascades Volcano Observatory, 1300 SE Cardinal Ct S100, Vancouver, Washington 98683, USA-
crisitem.classification.parent01. Atmosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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