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Further evidence of fractal structure in hydraulic conductivity distributions

✍ Scribed by Molz, Fred J.; Boman, Gerald K.

Book ID
119693172
Publisher
American Geophysical Union
Year
1995
Tongue
English
Weight
372 KB
Volume
22
Category
Article
ISSN
1944-8007

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The hydraulic conductivity of unsaturated soils with constant volume is a function of the saturation degree or matric suction, and can be obtained based on currently available procedures. However, each procedure has its limitations and consequently cares should be taken in the selection of a proper