Electrical charging of volcanic plumes

Many explosive terrestrial volcanic eruptions are accompanied by lightning and other atmospheric electrical phenomena. The plumes produced generate large perturbations in the surface atmospheric electric potential gradient and high charge densities have been measured on falling volcanic ash particle...

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Main Authors: James, MR, Wilson, L, Lane, S, Gilbert, J, Mather, T, Harrison, R, Martin, R
Format: Journal article
Language:English
Published: 2008
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author James, MR
Wilson, L
Lane, S
Gilbert, J
Mather, T
Harrison, R
Martin, R
author_facet James, MR
Wilson, L
Lane, S
Gilbert, J
Mather, T
Harrison, R
Martin, R
author_sort James, MR
collection OXFORD
description Many explosive terrestrial volcanic eruptions are accompanied by lightning and other atmospheric electrical phenomena. The plumes produced generate large perturbations in the surface atmospheric electric potential gradient and high charge densities have been measured on falling volcanic ash particles. The complex nature of volcanic plumes (which contain gases, solid particles, and liquid drops) provides several possible charging mechanisms. For plumes rich in solid silicate particles, fractoemission (the ejection of ions and atomic particles during fracture events) is probably the dominant source of charge generation. In other plumes, such as those created when lava enters the sea, different mechanisms, such as boiling, may be important. Further charging mechanisms may also subsequently operate, downwind of the vent. Other solar system bodies also show evidence for volcanism, with activity ongoing on Io. Consequently, volcanic electrification under different planetary scenarios (on Venus, Mars, Io, Moon, Enceladus, Tethys, Dione and Triton) is also discussed. © 2008 Springer Science+Business Media B.V.
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spelling oxford-uuid:08d4371b-378a-429f-bc58-484faa30b57f2022-03-26T09:15:02ZElectrical charging of volcanic plumesJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:08d4371b-378a-429f-bc58-484faa30b57fEnglishSymplectic Elements at Oxford2008James, MRWilson, LLane, SGilbert, JMather, THarrison, RMartin, RMany explosive terrestrial volcanic eruptions are accompanied by lightning and other atmospheric electrical phenomena. The plumes produced generate large perturbations in the surface atmospheric electric potential gradient and high charge densities have been measured on falling volcanic ash particles. The complex nature of volcanic plumes (which contain gases, solid particles, and liquid drops) provides several possible charging mechanisms. For plumes rich in solid silicate particles, fractoemission (the ejection of ions and atomic particles during fracture events) is probably the dominant source of charge generation. In other plumes, such as those created when lava enters the sea, different mechanisms, such as boiling, may be important. Further charging mechanisms may also subsequently operate, downwind of the vent. Other solar system bodies also show evidence for volcanism, with activity ongoing on Io. Consequently, volcanic electrification under different planetary scenarios (on Venus, Mars, Io, Moon, Enceladus, Tethys, Dione and Triton) is also discussed. © 2008 Springer Science+Business Media B.V.
spellingShingle James, MR
Wilson, L
Lane, S
Gilbert, J
Mather, T
Harrison, R
Martin, R
Electrical charging of volcanic plumes
title Electrical charging of volcanic plumes
title_full Electrical charging of volcanic plumes
title_fullStr Electrical charging of volcanic plumes
title_full_unstemmed Electrical charging of volcanic plumes
title_short Electrical charging of volcanic plumes
title_sort electrical charging of volcanic plumes
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