“…The soil water content was measured at matric potentials of −10, −40, −70, −100, −300, −700, −1000, −5000, and −15,000 cm H 2 O, and then, the values of parameters r , s , ␣ and n were estimated by the RETC code (Van Genuchten et al, 1991). We used the fitted RETC parameters as a starting value to perform an inversion for the hydraulic parameters based on the observed soil water content in NM in 2015 which has been reported in Chen et al (2017). The measured and inversed soil hydrualic parameters were shown in Table 2.…”