Polder Effects on Sediment-to-Soil Conversion: Water Table, Residual Available Water Capacity, and Salt Stress Interdependence

<table>Evolution of the CE<sub>1/5</sub> profiles according to the topographic level and thickness of leached soil surface (undrained grassland). The mound is due to sediment and soil deposited during the successive channel cleaning works. Low and high water tables indicate the domain of water table variation during the seasons.</table>

The Scientific World Journal

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Figure 7

Figure 7: Polder Effects on Sediment-to-Soil Conversion: Water Table, Residual Available Water Capacity, and Salt Stress Interdependence 