The size of an alluvial river channel can adjust in response to changes in the pattern of flows that it carries. An important case of such channel change occurs downstream of dams or water diversions where flow regulation has been observed to cause morphological and ecological impacts. (For complete abstract open document)
| Identifer | oai:union.ndltd.org:ADTP/245289 |
| Creators | Tilleard, John W. |
| Source Sets | Australiasian Digital Theses Program |
| Language | English |
| Detected Language | English |
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