Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5537
DC Field | Value | Language |
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dc.contributor.authorall | Spampinato, Letizia; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Salerno, G.G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Martin, R.S.; Department of Earth Sciences, University of Cambridge, UK | en |
dc.contributor.authorall | Sawyer, G.M.; Laboratoire Pierre Süe, CNRS-CEA, CE-Saclay, Fr. | en |
dc.contributor.authorall | Ramírez, C.; Centro de Investigaciones Geofisicas, University of Costa Rica (UCR), San Jose’, Costa Rica. | en |
dc.contributor.authorall | Ilyinskaya, E.; Department of Geography, University of Cambridge, UK | en |
dc.contributor.authorall | Oppenheimer, C.; Department of Geography, University of Cambridge, UK | en |
dc.date.accessioned | 2010-01-12T11:01:20Z | en |
dc.date.available | 2010-01-12T11:01:20Z | en |
dc.date.issued | 2009-12 | en |
dc.identifier.uri | http://hdl.handle.net/2122/5537 | en |
dc.description.abstract | We report results from a multidisciplinary campaign carried out at Poás crater-lake (Costa Rica) on 17-18 March 2009. Thermal imagery of fumaroles on the north side of the dome and the lake surface revealed mean apparent temperatures of 25-40°C (maximum of 80°C), and 30-35°C (maximum of 48°C), respectively. Mean radiative heat output of the lake, uncorrected for downwelling flux, was estimated as ~230 MW. The mean SO2 flux emitted by the crater measured by walking-traverses was 76 tonnes day-1, with approximately equal contributions from both the dome and the lake and fumarole plumes. Gas measurements by active open-path FTIR spectroscopy indicated molar ratios of H2O/SO2 = 151 and CO2/SO2 = 1.56. HCl and HF were not detected in measured spectra but based on the detection limits of these species, we calculate SO2/HCl > 40, and SO2/HF > 200. Particles were sampled from the plume by air filtration. The filters were analysed using ion chromatography, which revealed an abundance of K+ and SO42-, with smaller amounts of Ca2+, Mg2+ and Cl-. We discuss here the implications of the results for degassing pathways through the shallow magmatic-hydrothermal system. | en |
dc.language.iso | English | en |
dc.relation.ispartof | American Geophysical Union | en |
dc.subject | Thermal imagery, SO2 flux traverses, FTIR measurements, Particle composition, | en |
dc.subject | Poás volcano | en |
dc.title | Degassing pathways through the shallow magmatic-hydrothermal system of Poás | en |
dc.type | Poster session | en |
dc.description.status | Published | en |
dc.subject.INGV | 03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systems | en |
dc.description.ConferenceLocation | San Francisco, USA | en |
dc.description.obiettivoSpecifico | 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani | en |
dc.description.fulltext | open | en |
dc.contributor.author | Spampinato, Letizia | en |
dc.contributor.author | Salerno, G.G. | en |
dc.contributor.author | Martin, R.S. | en |
dc.contributor.author | Sawyer, G.M. | en |
dc.contributor.author | Ramírez, C. | en |
dc.contributor.author | Ilyinskaya, E. | en |
dc.contributor.author | Oppenheimer, C. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Department of Earth Sciences, University of Cambridge, UK | en |
dc.contributor.department | Laboratoire Pierre Süe, CNRS-CEA, CE-Saclay, Fr. | en |
dc.contributor.department | Centro de Investigaciones Geofisicas, University of Costa Rica (UCR), San Jose’, Costa Rica. | en |
dc.contributor.department | Department of Geography, University of Cambridge, UK | en |
item.openairetype | Poster session | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Department of Earth Sciences, University of Cambridge, UK. | - |
crisitem.author.dept | Department of Geography, University of Cambridge | - |
crisitem.author.dept | Centro de Investigaciones Geofisicas, University of Costa Rica (UCR), San Jose’, Costa Rica. | - |
crisitem.author.orcid | 0000-0002-0809-9135 | - |
crisitem.author.orcid | 0000-0002-9336-107X | - |
crisitem.author.orcid | 0000-0002-3663-9506 | - |
crisitem.author.orcid | 0000-0003-4506-7260 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 03. Hydrosphere | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Conference materials |
Files in This Item:
File | Description | Size | Format | |
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Spampinato et al., 2009.pdf | Conference abstract | 97.17 kB | Adobe PDF | View/Open |
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