A model of channel response in disturbed alluvial channels
Earth Surface Processes and Landforms
By: A. Simon
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Abstract
Dredging and straightening of alluvial channels between 1959 and 1978 in West Tennessee caused a series of morphologic changes along modified reaches and tributary streams. Degradation occurred for 10 to 15 years at sites upstream of the area of maximum disturbance and lowered bed-levels by as much as 6.1 m. Following degradation, reaches upstream of the area of maximum disturbance experienced a secondary aggradation phase in response to excessive incision and gradient reduction. -from Author
Suggested Citation
Simon, A., 1989, A model of channel response in disturbed alluvial channels: Earth Surface Processes and Landforms, v. 14, no. 1, p. 11-26, https://doi.org/10.1002/esp.3290140103.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | A model of channel response in disturbed alluvial channels |
| Series title | Earth Surface Processes and Landforms |
| DOI | 10.1002/esp.3290140103 |
| Volume | 14 |
| Issue | 1 |
| Publication Date | July 18, 2006 |
| Year Published | 1989 |
| Language | English |
| Publisher | Wiley |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Earth Surface Processes and Landforms |
| First page | 11 |
| Last page | 26 |