Lateral moisture flow beneath a sandy hillslope without an apparent impeding layer
Author:
Publisher
Wiley
Subject
Water Science and Technology
Reference30 articles.
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2. The influence of low-angled topography on hillslope soil-water convergence and stream discharge
3. 1971. ‘Three-dimensional transient, saturated-unsaturated flow in a groundwater basin’.
4. The mechanism of natural ground-water recharge and discharge: 2. Laboratory column experiments and field measurements
5. , and 1984. Lateral moisture movements in unsaturated anisotropic media, Purdue Univ., Lafayette, IN, Water Resources Research Center, TR No. 169, 105 pp.
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