Interactive Effects of Microbial Fertilizer and Soil Salinity on the Hydraulic Properties of Salt-Affected Soil.

As depicted in Figure 2 a–c, the water content of all the treatments presented a decreasing trend with an increase in soil water suction, which decreases sharply before 0.5 bar (100 kPa) and, subsequently, changes more slowly at 1–15 bar (100 kPa).

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