One Dimensional Water Flow through Snow.
A theory is developed to describe the percolation of water through isothermal snow with a vertical porosity gradient. While the necessary laboratory experiments have not been done for snow, concepts from the general theory of two phase flow through porous media are used in the development. The gener...
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| Format: | Text |
| Language: | English |
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1971
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| Online Access: | http://www.dtic.mil/docs/citations/AD0730304 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0730304 |