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

Table 1

Chemical compositions (in mg/L) of the waters pumped in January and February 2009 in the piezometers K1A-B (2.00 and 3.00 m), K2A-B (2.00 and 6.00 m), K3A-B (2.00 and 3.00 m), and K3C-D (2.00).

	Cl^−	Na	Ca	K	Mg	S	SO4	Total salinity (mg/L)
January piezometer
K1A-B (3.0 m)	4080	2508	361.1	116.6	339.4	756	2269	9673.9
K2A-B (6.0 m)	8370	4438	247.5	208.4	355.5	506	1517	15136.5
K3A-B (3.0 m)	4960	3059	301.8	154.8	513.2	1063	3189	12178.2
K1A-B (2.0 m)	1640	1302	330	61.16	199.1	427	1282	4814.16
K2A-B (2.0 m)	430	390	190.5	24.02	66.09	191	573	1673.51
K3A-B (2.0 m)	1980	1760	580.8	97.51	253.5	790	2369	7040.71
K3C-D (2.0 m)	970	1098	594.4	61.2	144.1	527	1580	4447.8
February piezometer
K1A-B (3.0 m)	2207	1797	292.5	86.59	242.3	543.2	1629.6	6254.99
K2A-B (6.0 m)	7201	4203	230.8	193.7	467.7	455	1365	13661.2
K3A-B (3.0 m)	3578	2643	435.9	128.8	431.4	821	2463	9680.1
K1A-B (2.0 m)	825	683	263.1	38.84	131.3	303.7	911.1	2852.34
K2A-B (2.0 m)	631	514.6	218.7	23.48	76.93	197.5	592.5	2075.21
K3A-B (2.0 m)	2661	2057	448.1	107.7	356.8	837.3	2511.9	8142.5
K3C-D (2.0 m)	834	1068	265.3	56.48	139.2	530.2	1590.6	3953.58