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- W2615172260 abstract "Abstract Field studies in the Song Hau distributary of the Mekong Delta in Vietnam conducted at high (Sept.-Oct 2014) and low (March 2015) Mekong River discharge are utilized to examine channel bottom morphology and links with sediment transport in the system. Multibeam bathymetric mapping surveys over the entire channel complex in the lower 80 km of the distributary channel, and over 12- to 24-h tidal periods at six transect locations in the reach are used to characterize bottom type and change on seasonal and tidal timescales, supplemented by bottom sampling. The results of this study indicate that the largest proportion of channel floor (up to 80% of the total area) is composed of substratum outcrops of relict sediment units deposited during the progradation of the delta in the last 3.5 ka. These take the form of outcrops that are either (1) steep-sided, tabular channel floor, (2) steep-sided sidewall, or (3) relatively flat channel floor. Flatter outcrops of channel floor substratum are identified by the presence of sedimentary furrows (" @default.
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- W2615172260 date "2017-09-01" @default.
- W2615172260 modified "2023-10-15" @default.
- W2615172260 title "Bottom morphology in the Song Hau distributary channel, Mekong River Delta, Vietnam" @default.
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- W2615172260 doi "https://doi.org/10.1016/j.csr.2017.05.010" @default.
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