3. Water retention properties
3.1 General
The ability of unsaturated soils to attract and retain water is quantified by the determination of water retention curves, an essential characteristic. These curves are determined by subjecting a sample to a cycle of drying and rewetting, applying stages of increasing and then decreasing suction, usually using the Richards cell. At each stage, the water content is measured by cancelling the air pressure within the cell to quickly remove the sample to be weighed; the sample is then placed back in the cell to be subjected to the next suction stage, by applying another air pressure that will generate either infiltration, if lower (rewetting path), or drainage, if higher (drying path). Water retention curves are obtained by plotting water content values in a "logarithm of suction/water...
Exclusive to subscribers. 97% yet to be discovered!
You do not have access to this resource.
Click here to request your free trial access!
Already subscribed? Log in!
The Ultimate Scientific and Technical Reference
This article is included in
Soil mechanics and geotechnics
This offer includes:
Knowledge Base
Updated and enriched with articles validated by our scientific committees
Services
A set of exclusive tools to complement the resources
Practical Path
Operational and didactic, to guarantee the acquisition of transversal skills
Doc & Quiz
Interactive articles with quizzes, for constructive reading
Water retention properties