Contributions to storm quickflow in a small headwater catchment—the role of natural pipes and soil macropores

Contributions to storm quickflow in a small headwater catchment—the role of natural pipes and... Analysis of hydrographs from a 4·3 hectare stream head catchment indicates that storm runoff is generated from dynamic source areas. The volume and timing of contributions from different parts of the catchment show, when compared with the extent of surface saturation, that pipeflow generated from areas not saturated at the soil surface is a significant component of the quickflow hydrograph. A simple model of pipeflow generation and contribution is discussed in the light of field results. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Earth Surface Processes and Landforms Wiley

Contributions to storm quickflow in a small headwater catchment—the role of natural pipes and soil macropores

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Publisher
Wiley
Copyright
Copyright © 1983 John Wiley & Sons, Ltd
ISSN
0197-9337
eISSN
1096-9837
DOI
10.1002/esp.3290080306
Publisher site
See Article on Publisher Site

Abstract

Analysis of hydrographs from a 4·3 hectare stream head catchment indicates that storm runoff is generated from dynamic source areas. The volume and timing of contributions from different parts of the catchment show, when compared with the extent of surface saturation, that pipeflow generated from areas not saturated at the soil surface is a significant component of the quickflow hydrograph. A simple model of pipeflow generation and contribution is discussed in the light of field results.

Journal

Earth Surface Processes and LandformsWiley

Published: May 1, 1983

References

  • An experimental investigation of runoff production in permeable soils
    Dunne, Dunne; Black, Black

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