1887

Abstract

The infiltration rate in soils is important for determining the propagation of saturation, and hence for the stability of slopes subjected to overrunning water. The paper suggests a simple practical formula for interpretation of infiltration tests, validated by various laboratory and field test results.

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/content/papers/10.3997/2214-4609-pdb.150.B06
2010-01-20
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.150.B06
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