Laboratory analogues of Martian electrostatic discharges

Electrical discharges in Martian analogue materials have previously been generated by agitation of the material in a low-pressure carbon dioxide environment. These results have led to the supposition that lightning is likely on Mars, on the basis that the surface material becomes triboelectrically c...

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Κύριοι συγγραφείς: Aplin, K, Goodman, T, Herpoldt, K, Davis, C
Μορφή: Journal article
Γλώσσα:English
Έκδοση: 2012
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author Aplin, K
Goodman, T
Herpoldt, K
Davis, C
author_facet Aplin, K
Goodman, T
Herpoldt, K
Davis, C
author_sort Aplin, K
collection OXFORD
description Electrical discharges in Martian analogue materials have previously been generated by agitation of the material in a low-pressure carbon dioxide environment. These results have led to the supposition that lightning is likely on Mars, on the basis that the surface material becomes triboelectrically charged, and the charges are then gravitationally separated in dust storms. We have reproduced one of these experiments and find that triboelectric charging of the Martian regolith simulant by the walls of the vessel used can adequately explain all the effects observed. Our results indicate that unless special care is taken to avoid wall effects, the electrostatic properties of a laboratory system cannot be extrapolated to the Martian environment. We also note that charging of the outside of the vessel used can generate transients within the vessel which could be mistaken for electrical discharge signals, unless accompanied by optical emissions. © 2012 Elsevier Ltd. All rights reserved.
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spelling oxford-uuid:17a2196d-a6fe-4b41-a814-1f9f2be37d252022-03-26T10:38:35ZLaboratory analogues of Martian electrostatic dischargesJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:17a2196d-a6fe-4b41-a814-1f9f2be37d25EnglishSymplectic Elements at Oxford2012Aplin, KGoodman, THerpoldt, KDavis, CElectrical discharges in Martian analogue materials have previously been generated by agitation of the material in a low-pressure carbon dioxide environment. These results have led to the supposition that lightning is likely on Mars, on the basis that the surface material becomes triboelectrically charged, and the charges are then gravitationally separated in dust storms. We have reproduced one of these experiments and find that triboelectric charging of the Martian regolith simulant by the walls of the vessel used can adequately explain all the effects observed. Our results indicate that unless special care is taken to avoid wall effects, the electrostatic properties of a laboratory system cannot be extrapolated to the Martian environment. We also note that charging of the outside of the vessel used can generate transients within the vessel which could be mistaken for electrical discharge signals, unless accompanied by optical emissions. © 2012 Elsevier Ltd. All rights reserved.
spellingShingle Aplin, K
Goodman, T
Herpoldt, K
Davis, C
Laboratory analogues of Martian electrostatic discharges
title Laboratory analogues of Martian electrostatic discharges
title_full Laboratory analogues of Martian electrostatic discharges
title_fullStr Laboratory analogues of Martian electrostatic discharges
title_full_unstemmed Laboratory analogues of Martian electrostatic discharges
title_short Laboratory analogues of Martian electrostatic discharges
title_sort laboratory analogues of martian electrostatic discharges
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