Fluvial Processes In River Engineering Downloads Torrent ^HOT^
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A fact that is worth highlighting in Figure 12 is that, despite the existence of a clear trend in the net loss of delta-plain area for some deltas (Figure 12e), this trend is generally not accompanied by a decrease in the magnitude of bedload sediment flux, with the exception of the Niger (Figure 12c). This suggests that the reduction in delta area is not only due to the direct effect of fluvial sediment loss. We feel that this is likely caused by changes in the fluvial sediment flux associated with increasing riverine discharge. In addition, dredging operations have also been used in the upper Rhine and Rhone, and this likely contributed to an increase in sediment flux in the upper parts of these rivers. A distinct and noteworthy feature is that in the case of the Po and Ebro deltas, in particular, the delta-plain areas have actually increased slightly post-dam, which may be related to the effect of new dams. There is, at present, an absence of data available to evaluate this hypothesis. In the case of the Ceyhan, the net loss of delta-plain area appears to be due, at least partially, to the general reduction in fluvial sediment load due to dam construction (Cetin et al., 1999; Pfeffer and Ekercin, 2012; Ataol, 2015). This is in line with an earlier modelling study carried out by Tessier et al. (2013), which found that the loss of fluvial sediment load in the Ceyhan delta is likely to have occurred before the construction of the main dam. This study also suggested that, similar to the Rhone delta, beach erosion may also be important in the Ceyhan delta (Tessier et al., 2013). A significant increase in the volume of beach erosion (Figure 13a) is observed after dam construction (Tessier et al., 2013), in line with the hypothesis that the reduction in fluvial sediment load occurs first, then subsequently leads to the loss of area in the delta, and the excess of sediment on beaches. Beach sedimentation is a process where the main grains that remain in the delta after fluvial sedimentation are transported to the beaches, but where the freshwater sediment is transported a considerable distance. Tessier et al. (2013) suggested that this process should therefore be considered in the Ceyhan delta, in addition to the effects of the dam (Tessier et al., 2013).
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