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Application of geophysical methods in describing spatial variability of saturated hydraulic conductivity in the zone of aeration

✍ Scribed by O. Mazáč; M. Císlerová; T. Vogel

Book ID
115971571
Publisher
Elsevier Science
Year
1988
Tongue
English
Weight
484 KB
Volume
103
Category
Article
ISSN
0022-1694

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The time required at a field site to obtain a few measurements of saturated hydraulic conductivity (K s ) will allow for many measurements of soil air permeability (k a ). This study investigates if k a measured in situ (k a,in situ ) can be a substitute for measurement of K s in relation to infiltr