Impact of Cooling on Water and Salt Migration of High-Chlorine Saline Soils

Table 4

Numerical simulation parameter and boundary conditions.

Soil type	Constitutive parameters			Residual water content	Saturated water content	Permeability coefficient (m^2·s^−1)	Constant	Boundary temperature (°C)
								Top	Bottom
Silty clay	2.65	0.25	0.5	0	0.42	10^−7	0.47	−10	5