Surface-sediment grain-size distribution and sediment transport in the subaqueous Mekong Delta, Vietnam

Thanh Trung Nguyen1, Karl Stattegger2, Charles (Chuck) Nittrouer3, Phach Van Phung1, Paul Liu4, David John DeMaster4, Dung Viet Bui5, Anh Duc Le1 and Tien Ngoc Nguyen1, (1)Institute of Marine Geology and Geophysics, Ha Noi, Vietnam, (2)University of Kiel, Kiel, Germany, (3)University of Washington, Seattle, WA, United States, (4)North Carolina State Univ, Raleigh, NC, United States, (5)Vietnam Petroleum Institute, Ha Noi, Vietnam
Abstract:
Collected surface-sediment samples in coastal water around Mekong Delta (from distributary channels to Ca Mau Peninsula) were analyzed to determine surface-sediment grain-size distribution and sediment-transport trend in the subaqueous Mekong Delta. The grain-size data set of 238 samples was obtained by using the laser instrument Mastersizer 2000 and LS Particle Size Analyzer. Fourteen samples were selected for geochemical analysis (total-organic and carbonate content). These geochemical results were used to assist in interpreting variations of granulometricparamenters along the cross-shore transects. Nine transects were examined from CungHau river mouth to Ca Mau Peninsula and six thematic maps on the whole study area were made. The research results indicate that: (1) generally, the sediment becomes finer from the delta front downwards to prodelta and becomes coarser again and poorer sorted on the adjacent inner shelf due to different sources of sediment; (2) sediment-granulometry parameters vary among sedimentary sub-environments of the underwater part of Mekong Delta, the distance from sediment source and hydrodynamic regime controlling each region; (3) the net sediment transport is southwest toward the Ca Mau Peninsula.