Polder Effects on Sediment-to-Soil Conversion: Water Table, Residual Available Water Capacity, and Salt Stress Interdependence
Figure 3
(a) Typical structure revealed by the long resistivity sections in geoelectrical prospecting, (b) schematic representation of the bri structure from the peripheral limestone contact to the inner “dry marsh.” (1) Surface layer impacted by the desiccation-shrinkage effects, (2) to evolution due to the reclaiming and desiccation effect, and (3) to consolidation in depth.
