Special Section: Chapman Conference on Hydrogeochemical Responses of Forested Catchments
Preferential Flow and the Generation of Runoff: 1. Boundary Layer Flow Theory
Article first published online: 9 JUL 2010
Copyright 1990 by the American Geophysical Union.
Water Resources Research
Volume 26, Issue 12, pages 3055–3063, December 1990
How to Cite
1990), Preferential Flow and the Generation of Runoff: 1. Boundary Layer Flow Theory, Water Resour. Res., 26(12), 3055–3063, doi:10.1029/WR026i012p03055.(
- Issue published online: 9 JUL 2010
- Article first published online: 9 JUL 2010
- Manuscript Accepted: 3 JUL 1990
- Manuscript Received: 14 NOV 1989
Approaches to soil water flow, which are based on the theory of potential flow, often overestimate either the volume of flow or the response time at the hillslope scale when their results are compared with observations. Macropore flow is frequently thought to be the reason for the discrepancy between observations and model performance. The expression macropore flow is considered to be too restricting. It confines the rapid flow and transport processes to the easily observed channels, concealing the more general question as to what degree potential flow theory adequately describes flow in porous media. The application of potential flow theory to infiltration leads to the Richards equations only when hydrodynamic dispersion of soil water and capillary potential are perfectly correlated. In this paper a boundary layer infiltration model is presented, which is based on kinematic theory. It is also expanded to lateral flow in a sloping soil.