Geometric modeling of Holocene large-river delta growth patterns, as constrained by environmental settings

Topographic/bathymetric conditions of the continental shelf can significantly influence the long-term growth of river deltas. In particular, these conditions constrain the accommodation space for sedimentation in the deltaic areas. In this study, we use a conceptual geometric model to evaluate the role played by this factor, on the basis of the principle of mass conservation. The Ganges-Brahmaputra, Mekong and Nile deltas are examined as three typical examples, in terms of their different original seabed morphologies. The control variate method is applied to eliminate the effect of the difference in model input variables. The results show that, assuming a constant sediment load, the delta growth rate will decrease with time; a higher value of the original seabed slope leads to a lower shoreline progradation rate for the subaerial delta and a higher growth rate for the subaqueous delta. Thus, the original seabed morphology represented by slope is a critical factor affecting the evolution of Holocene large-river deltas. These results explain the interrelationships between sediment load, deltaic plain area, and the original seabed slopes for the 27 large-river deltas worldwide, located in the middle/low latitudes, with different tectonic backgrounds. In the future, the conceptual geometric model may be combined with sediment dynamic modeling to identify more details of the evolution of these deltas.

Automated summary

The topographic/bathymetric conditions of the continental shelf play a significant role in influencing the long-term growth of river deltas, with the original seabed morphology being a critical factor affecting delta evolution. The study shows that with a constant sediment load, delta growth rate decreases over time, and higher original seabed slope leads to lower shoreline progradation rate for subaerial deltas and higher growth rate for subaqueous deltas. This research highlights the importance of considering the interrelationships between sediment load, deltaic plain area, and original seabed slopes in understanding the evolution of large-river deltas.