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Longitudinal profile of channels cut by springs

Author(s)
Devauchelle, Olivier; Petroff, A. P.; Lobkovsky, Alexander E.; Rothman, Daniel H.
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Abstract
We propose a simple theory for the longitudinal profile of channels incised by groundwater flow. The aquifer surrounding the stream is represented in two dimensions through Darcy's law and the Dupuit approximation. The model is based on the assumption that, everywhere in the stream, the shear stress exerted on the sediment by the flow is close to the minimal intensity required to displace a sand grain. Because of the coupling of the stream discharge with the water table elevation in the neighbourhood of the channel head, the stream elevation decreases as the distance from the stream's tip with an exponent of 2/3. Field measurements of steephead ravines in the Florida Panhandle conform well to this prediction.
Date issued
2010-12
URI
http://hdl.handle.net/1721.1/74044
Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Journal
Journal of Fluid Mechanics
Publisher
Cambridge University Press
Citation
Devauchelle, O. et al. “Longitudinal Profile of Channels Cut by Springs.” Journal of Fluid Mechanics 667 (2010): 38–47. © Cambridge University Press 2010
Version: Final published version
ISSN
0022-1120
1469-7645

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