Fig. 14From: Gravity changes associated with variations in local land-water distributions: Observations and hydrological modeling at Isawa Fan, northern JapanDependency of soil moisture distributions and gravity changes on b. For b equal to (1) 0.000, (2) 2.000, (3) 3.947 (default value: thick line), (4) 6.000, (5) 8.000. (a) Steady-state soil moisture profile with p = 1.0, θs(Z; p = 1). (b) Time variation of soil moisture at 50 cm below the ground surface with p = 1.0, θ(zs − 0.5 t; p = 1). (c) Gravity changes due to soil moisture distribution, gw(t).Back to article page