Polder Effects on Sediment-to-Soil Conversion: Water Table, Residual Available Water Capacity, and Salt Stress Interdependence
Figure 11
Evolution of the tensiometer pressures and gravimetric water contents at 40, 60, and 80 cm depth from 01 April 2011 to 15 July 2011 in the grassland. The d40 and d60 indicate the disconnection of the porous plugs at the depths of 40 and 60 cm, respectively.
