Hydraulic conductivity and sorptivity at unsaturated and saturated conditions as related to water infiltration in soils
Sorptivity (S) has been defined in terms of the horizontal infiltration equation. At unsaturated conditions (at a very short time) S represents “maximum sorption capacity”, but in saturated conditions the sorption capacity decreases with the time. Over a long time of infiltration, sorptivity was not...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Federation of Eurasian Soil Science Societies
2020-01-01
|
| Series: | Eurasian Journal of Soil Science |
| Subjects: | |
| Online Access: | http://ejss.fesss.org/10.18393/ejss.621759 |