Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning

Evidence for the existance of volcanic lightning is produced from a literature survey and the charge sources which have been suggested are listed and those, of the 18th and 19th centuries, which involved boiling water are reviewed in detail. Studies of saline contact charging, undertaken by Blanchar...

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Main Author: Pounder, Colin
Format: Thesis
Language:unknown
Published: 1979
Subjects:
Online Access:https://oro.open.ac.uk/54206/
https://oro.open.ac.uk/54206/1/469319.pdf
https://doi.org/10.21954/ou.ro.0000d3be
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spelling ftopenunivgb:oai:oro.open.ac.uk:54206 2023-06-11T04:17:11+02:00 Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning Pounder, Colin 1979 application/pdf https://oro.open.ac.uk/54206/ https://oro.open.ac.uk/54206/1/469319.pdf https://doi.org/10.21954/ou.ro.0000d3be unknown https://oro.open.ac.uk/54206/1/469319.pdf Pounder, Colin (1979). Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning. PhD thesis The Open University. Thesis Public PeerReviewed 1979 ftopenunivgb https://doi.org/10.21954/ou.ro.0000d3be 2023-05-28T05:57:00Z Evidence for the existance of volcanic lightning is produced from a literature survey and the charge sources which have been suggested are listed and those, of the 18th and 19th centuries, which involved boiling water are reviewed in detail. Studies of saline contact charging, undertaken by Blanchard et al, when Surtsey emerged in 1963 are reviewed and lead to the continuation, in this investigation, of the Leidenfrost form of boiling and the discovery of an associated charging process. This discovery resolves a two centuries long dispute as to whether the Leidenfrost phenomenon of boiling produces charge as well as showing its important relevance to volcanic lightning where solution contact charging is in evidence. The mechanisms by which charged particles are emitted and formed into hollow solute spheres have been investigated and their charge and size distributions determined. Their structure has been compared with the structure of particles produced by flash boiling and spraying of saline solution. The energy conversion involved in the particle emission mechanism has also been studied. Charging mechanisms and some charging processes have been reviewed and by comparing results from other investigations speculations as to which mechanisms produce charge in the Leidenfrost process have been attempted. The comparison of results leads to the suggestion that Blanchard's observations are more likely to be Leidenfrost boiling than, as he assumed, flash boiling. The high average charge per particle of 10 -14 C on particles from Leidenfrost boiling indicate that the number density is smaller, by a factor of 10 4 , than that previously suggested to produce the fields measured in volcanic clouds. Exploratory experiments have established that in addition to saline solution other aqueous solutions will also produce charge. Thesis Surtsey The Open University: Open Research Online (ORO) Blanchard ENVELOPE(-62.083,-62.083,-64.733,-64.733) Surtsey ENVELOPE(-20.608,-20.608,63.301,63.301)
institution Open Polar
collection The Open University: Open Research Online (ORO)
op_collection_id ftopenunivgb
language unknown
description Evidence for the existance of volcanic lightning is produced from a literature survey and the charge sources which have been suggested are listed and those, of the 18th and 19th centuries, which involved boiling water are reviewed in detail. Studies of saline contact charging, undertaken by Blanchard et al, when Surtsey emerged in 1963 are reviewed and lead to the continuation, in this investigation, of the Leidenfrost form of boiling and the discovery of an associated charging process. This discovery resolves a two centuries long dispute as to whether the Leidenfrost phenomenon of boiling produces charge as well as showing its important relevance to volcanic lightning where solution contact charging is in evidence. The mechanisms by which charged particles are emitted and formed into hollow solute spheres have been investigated and their charge and size distributions determined. Their structure has been compared with the structure of particles produced by flash boiling and spraying of saline solution. The energy conversion involved in the particle emission mechanism has also been studied. Charging mechanisms and some charging processes have been reviewed and by comparing results from other investigations speculations as to which mechanisms produce charge in the Leidenfrost process have been attempted. The comparison of results leads to the suggestion that Blanchard's observations are more likely to be Leidenfrost boiling than, as he assumed, flash boiling. The high average charge per particle of 10 -14 C on particles from Leidenfrost boiling indicate that the number density is smaller, by a factor of 10 4 , than that previously suggested to produce the fields measured in volcanic clouds. Exploratory experiments have established that in addition to saline solution other aqueous solutions will also produce charge.
format Thesis
author Pounder, Colin
spellingShingle Pounder, Colin
Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning
author_facet Pounder, Colin
author_sort Pounder, Colin
title Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning
title_short Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning
title_full Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning
title_fullStr Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning
title_full_unstemmed Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning
title_sort investigation of a reproducible boiling phenomenon with relevance to volcanic lightning
publishDate 1979
url https://oro.open.ac.uk/54206/
https://oro.open.ac.uk/54206/1/469319.pdf
https://doi.org/10.21954/ou.ro.0000d3be
long_lat ENVELOPE(-62.083,-62.083,-64.733,-64.733)
ENVELOPE(-20.608,-20.608,63.301,63.301)
geographic Blanchard
Surtsey
geographic_facet Blanchard
Surtsey
genre Surtsey
genre_facet Surtsey
op_relation https://oro.open.ac.uk/54206/1/469319.pdf
Pounder, Colin (1979). Investigation of a Reproducible Boiling Phenomenon with Relevance to Volcanic Lightning. PhD thesis The Open University.
op_doi https://doi.org/10.21954/ou.ro.0000d3be
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