Changes in gas composition prior to a minor explosive eruption at Masaya volcano, Nicaragua

A small explosive eruption at Masaya volcano on 23 April 2001, in which a number of people were injured, was preceded by a distinct change in plume gas compositions. Open-path Fourier transform infrared spectroscopy (FTS) measurements show that the SO2/HCl molar ratio increased from 1.8 to 4.6 betwe...

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Үндсэн зохиолчид: Duffell, H, Oppenheimer, C, Pyle, D, Galle, B, McGonigle, A, Burton, MR
Формат: Journal article
Хэвлэсэн: 2003
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author Duffell, H
Oppenheimer, C
Pyle, D
Galle, B
McGonigle, A
Burton, MR
author_facet Duffell, H
Oppenheimer, C
Pyle, D
Galle, B
McGonigle, A
Burton, MR
author_sort Duffell, H
collection OXFORD
description A small explosive eruption at Masaya volcano on 23 April 2001, in which a number of people were injured, was preceded by a distinct change in plume gas compositions. Open-path Fourier transform infrared spectroscopy (FTS) measurements show that the SO2/HCl molar ratio increased from 1.8 to 4.6 between April 2000 and April/May 2001. The SO2 flux decreased from 11 to 4 kg s-1 over this period. We interpret these changes to be the result of scrubbing of water-soluble magmatic gases by a rejuvenated hydrothermal system. A sequence of M 5 earthquakes with epicentres about 7 km from the volcano occurred in July 2000. These may have altered the fracture permeability close to the magmatic conduit, and caused increased magmatic-hydrothermal interaction, leading eventually to the phreatic explosion in 2001. Continuous FTS measurements at suitable volcanoes could provide useful information in support of eruption prediction and forecasting. © 2003 Elsevier Science B.V..
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spelling oxford-uuid:25ab1554-46ba-49b7-a9ed-40324c66df4c2022-03-26T11:56:45ZChanges in gas composition prior to a minor explosive eruption at Masaya volcano, NicaraguaJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:25ab1554-46ba-49b7-a9ed-40324c66df4cSymplectic Elements at Oxford2003Duffell, HOppenheimer, CPyle, DGalle, BMcGonigle, ABurton, MRA small explosive eruption at Masaya volcano on 23 April 2001, in which a number of people were injured, was preceded by a distinct change in plume gas compositions. Open-path Fourier transform infrared spectroscopy (FTS) measurements show that the SO2/HCl molar ratio increased from 1.8 to 4.6 between April 2000 and April/May 2001. The SO2 flux decreased from 11 to 4 kg s-1 over this period. We interpret these changes to be the result of scrubbing of water-soluble magmatic gases by a rejuvenated hydrothermal system. A sequence of M 5 earthquakes with epicentres about 7 km from the volcano occurred in July 2000. These may have altered the fracture permeability close to the magmatic conduit, and caused increased magmatic-hydrothermal interaction, leading eventually to the phreatic explosion in 2001. Continuous FTS measurements at suitable volcanoes could provide useful information in support of eruption prediction and forecasting. © 2003 Elsevier Science B.V..
spellingShingle Duffell, H
Oppenheimer, C
Pyle, D
Galle, B
McGonigle, A
Burton, MR
Changes in gas composition prior to a minor explosive eruption at Masaya volcano, Nicaragua
title Changes in gas composition prior to a minor explosive eruption at Masaya volcano, Nicaragua
title_full Changes in gas composition prior to a minor explosive eruption at Masaya volcano, Nicaragua
title_fullStr Changes in gas composition prior to a minor explosive eruption at Masaya volcano, Nicaragua
title_full_unstemmed Changes in gas composition prior to a minor explosive eruption at Masaya volcano, Nicaragua
title_short Changes in gas composition prior to a minor explosive eruption at Masaya volcano, Nicaragua
title_sort changes in gas composition prior to a minor explosive eruption at masaya volcano nicaragua
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