Delta lobe development in response to changing fluvial sediment supply by the second largest river in Vietnam

Abstract

While the importance of sediment supply to river delta evolution is well recognized, the extent to which sediment from upstream sources contributes to the subaerial and subaqueous components of its delta is not yet fully comprehended. To investigate this issue, the present study analyzed satellite images (Landsat) spanning from 1975 to present and nautical charts in different periods to examine the morphological evolution and its relationship with changes in river sediment loads of the Ba Lat delta lobe, located on the central coast of the second largest river system (Red) in Vietnam. We proposed a hybrid approach to estimate suspended sediment entering the sea via the Ba Lat mouth, based on a combination of one-line theory and long-term observation from a gauging station. The results show a significant reduction (∼91.5 %) in annual sediment load over the entire 64-year estimation period (1958–2021), which is associated with the operation of large dam-reservoirs upstream. The evolution of the Ba Lat delta lobe was found to be highly correlated with sediment load, with a huge sediment supply from the Red River causing the delta lobe to move seaward at a rate of more than 100 m/yr and the deltaic land area to accrete at a rate of 117 ha/yr between 1975 and 1990. However, since the early 1990s, the annual sediment flux has reduced of 57 %, resulting in more than 50 % of the delta lobe's shoreline experiencing severe erosion. The current amount of sediment load delivered to the sea (1.4 × 106 m3/yr) is insufficient to prograde the delta lobe, which could lead to continued land loss in the future. We attribute these erosions mainly to the reduced river sediment supply, generated by the large dam-reservoirs located upstream of the delta. The study suggests that these results and methods can inform coastal management and enhance understanding of delta lobe evolution by providing insights into changes in shoreline position, land area, and subaqueous component.