Movement of air through water in partly saturated soils

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TypeArticle
Journal titleNature
ISSN0028-0836
Volume212
Issue5069
Pages14631464; # of pages: 2
AbstractWhen the water content of a soil is reduced below saturation, the interfaces between air and water lie within pores, and are cuved because of surface tension. In many situations of geotechnical and agricultural interest the soil is partly saturated. In a sample of the soil the interfaces between the external air and the pore water are curved but localized near the surface.
Publication date
LanguageEnglish
AffiliationNRC Institute for Research in Construction; National Research Council Canada
Peer reviewedNo
IdentifierDBR-RP-316
NRC number9574
532
NPARC number20375422
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Record identifier91a7c779-d79f-47fd-8ec2-6e52600806ec
Record created2012-07-23
Record modified2016-05-09
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