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Moisture and energy conditions within sloping soil mass during drainage
To explain source of nonstorm streamflow in deep-soiled areas of southern Appalachians, in clining concrete trough was constructed on 40% slope; structure was packed with natural sandy-loam soil and after thorough soaking was covered with plastic to prevent evaporation; outflow was measured at base, and soil moisture tension and content were recorded for 145 days; expressions for outflow during 145 day period.
Moisture and energy conditions within sloping soil mass during drainage
To explain source of nonstorm streamflow in deep-soiled areas of southern Appalachians, in clining concrete trough was constructed on 40% slope; structure was packed with natural sandy-loam soil and after thorough soaking was covered with plastic to prevent evaporation; outflow was measured at base, and soil moisture tension and content were recorded for 145 days; expressions for outflow during 145 day period.
Moisture and energy conditions within sloping soil mass during drainage
J Geophysical Research
Hewlett, J.D. (author) / Hibbert, A.R. (author)
1963
7 pages
Article (Journal)
English
© Metadata Copyright Elsevier B. V. All rights reserved.
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