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Sediment transport in an active erodible channel bend of Brahmaputra river

✍ Scribed by Tapas Karmaker; Y. Ramprasad; Subashisa Dutta


Book ID
107590247
Publisher
Indian Academy of Sciences
Year
2010
Tongue
English
Weight
800 KB
Volume
35
Category
Article
ISSN
0256-2499

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Floodplain deposits are recognized as potentially large sinks for fluvial sediments, yet spatial and temporal patterns of accumulation are not known for many river systems. In the tectonically active Bengal Basin, the Ganges and Brahmaputra rivers coalesce and have formed a large floodplain=delta co