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Cited by 424

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The role of topography in controlling throughflow generation

Open access
Anderson, M. G., Burt, T. P.·1978·Earth Surface Processes

Abstract

Previous studies of the downslope movement of soil moisture have been largely confined to two‐dimensional slope profiles—the influence of contour curvature (three‐dimensional) on moisture movement has received little attention. An automatic tensiometer system has been used to monitor soil moisture status continuously in a single hollow and adjacent spurs. Maximum saturated hillslope flow is shown to coincide with the stream discharge ‘throughflow peak’. Relative to the hollow, little saturation is evident at the base of the spurs. This subcatchment model is applied to a major portion of the catchment, showing the general importance of topography in the control of stream discharge.

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Metadata

Authors
Anderson, M. G., & Burt, T. P.
Venue
Earth Surface Processes
Publisher
Wiley
Published
1978-10
Volume
3
Issue
4
Pages
331-344
ISSN
  • 0197-9337 (ISSN-L)
  • 0360-1269
  • 1931-8065
OpenAlex
W2076837330
Cited by
424
References
0
FWCI
41.30
Type
journal article
Language
en
Open access
green

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.