Fig. 9. Estimated hydraulic conductivity–water content relationship with Wind's method under infiltration conditions for the sandy soil. The parameter 
s is not estimated and set to its true value and the Ksat point is an independent measurement.
Fig. 9. Estimated hydraulic conductivity–water content relationship with Wind's method under infiltration conditions for the sandy soil. The parameter s is not estimated and set to its true value and the Ksat point is an independent measurement.