Convection in Drying and Freezing Ground
In this paper we analyse the drying of a soil composed of particles, water and solute impurities, and study the occurrence of convective instabilities during evaporation. We find that the main driving force for instability is the formation of a concentration gradient at the soil surface due to the e...
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| Online Access: | https://dx.doi.org/10.48550/arxiv.1210.1533 https://arxiv.org/abs/1210.1533 |
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ftdatacite:10.48550/arxiv.1210.1533 2023-05-15T14:56:29+02:00 Convection in Drying and Freezing Ground Faizal, Mir Peppin, Stephen 2012 https://dx.doi.org/10.48550/arxiv.1210.1533 https://arxiv.org/abs/1210.1533 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Geophysics physics.geo-ph FOS Physical sciences article-journal Article ScholarlyArticle Text 2012 ftdatacite https://doi.org/10.48550/arxiv.1210.1533 2022-04-01T13:42:52Z In this paper we analyse the drying of a soil composed of particles, water and solute impurities, and study the occurrence of convective instabilities during evaporation. We find that the main driving force for instability is the formation of a concentration gradient at the soil surface due to the evaporation of water. A similar phenomenon may occur during the thawing of frozen ground in Arctic regions. : 12 pages, 0 figures Text Arctic DataCite Metadata Store (German National Library of Science and Technology) Arctic |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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unknown |
| topic |
Geophysics physics.geo-ph FOS Physical sciences |
| spellingShingle |
Geophysics physics.geo-ph FOS Physical sciences Faizal, Mir Peppin, Stephen Convection in Drying and Freezing Ground |
| topic_facet |
Geophysics physics.geo-ph FOS Physical sciences |
| description |
In this paper we analyse the drying of a soil composed of particles, water and solute impurities, and study the occurrence of convective instabilities during evaporation. We find that the main driving force for instability is the formation of a concentration gradient at the soil surface due to the evaporation of water. A similar phenomenon may occur during the thawing of frozen ground in Arctic regions. : 12 pages, 0 figures |
| format |
Text |
| author |
Faizal, Mir Peppin, Stephen |
| author_facet |
Faizal, Mir Peppin, Stephen |
| author_sort |
Faizal, Mir |
| title |
Convection in Drying and Freezing Ground |
| title_short |
Convection in Drying and Freezing Ground |
| title_full |
Convection in Drying and Freezing Ground |
| title_fullStr |
Convection in Drying and Freezing Ground |
| title_full_unstemmed |
Convection in Drying and Freezing Ground |
| title_sort |
convection in drying and freezing ground |
| publisher |
arXiv |
| publishDate |
2012 |
| url |
https://dx.doi.org/10.48550/arxiv.1210.1533 https://arxiv.org/abs/1210.1533 |
| geographic |
Arctic |
| geographic_facet |
Arctic |
| genre |
Arctic |
| genre_facet |
Arctic |
| op_rights |
arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ |
| op_doi |
https://doi.org/10.48550/arxiv.1210.1533 |
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