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Kinematic subsurface stormflow
Abstract
This paper builds on the analysis of Henderson and Wooding (1964) in comparing simplified models of subsurface stormflow for the case of a sloping soil mantle in which the hydraulic conductivity is constant throughout. It is shown that models based on a kinematic wave formulation may be good approximations for those based on the extended Dupuit‐Forchheimier assumptions for values of the nondimensional parameter λ = 4 i cos θ/(K sin 2 θ) less than about 0.75 in terms of predicting both water table profiles and subsurface stormflow hydrographs. By using this critical value of λ the range of values of slope angle and saturated hydraulic conductivity for which the kinematic approximation is valid can be specified. A comparison is made with slope angles and hydraulic conductivities at field sites where subsurface stormflow has been shown to be an important component of catchment storm response. It is concluded that the kinematic approximation may be useful for cases of practical interest.
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Citations
Cited by
Gerke, H. H., & van Genuchten, M. T. (1993) · Water Resources Research · doi:10.1029/92wr02339 · Cited by 1,247
Macropores and water flow in soils revisited: REVIEW
Beven, K., & Germann, P. (2013) · Water Resources Research · doi:10.1002/wrcr.20156 · Cited by 916
Self-citationA Distributed Slope Stability Model for Steep Forested Basins
Wu, W., & Sidle, R. C. (1995) · Water Resources Research · doi:10.1029/95wr01136 · Cited by 657
Storm Runoff Generation in Humid Headwater Catchments: 1. Where Does the Water Come From?
Pearce, A. J., Stewart, M. K., & Sklash, M. G. (1986) · Water Resources Research · doi:10.1029/wr022i008p01263 · Cited by 462
McDonnell, J. J., & Beven, K. (2014) · Water Resources Research · doi:10.1002/2013wr015141 · Cited by 462
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Metadata
- Authors
- Beven, K.
- Venue
- Water Resources Research
- Publisher
- American Geophysical Union (AGU)
- Published
- 1981-10
- Volume
- 17
- Issue
- 5
- Pages
- 1419-1424
- ISSN
- 0043-1397 (ISSN-L)
- 1944-7973
- OpenAlex
- W2125488703
- Cited by
- 244
- References
- 0
- FWCI
- 8.39
- Type
- journal article
- Language
- en
- Open access
- closed
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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