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Averaged water potentials in soil water and groundwater, and their connection to menisci in soil pores, field scale flow phenomena, and simple groundwater flows

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Figure

Fig. 1. A hypothetical liquid-filled pore with a single exit in whichizontal liquid-filled cross-sectionthe liquid-gas interface is located at vertical position x∗3
Table 1. Amount of water needed to bring the phreatic level up to the soil surface when initially the capillary fringe extends to the soilsurface, and the time needed to deliver this water during rainfall of moderate intensity
Fig. 3. Two of the three groundwater flow cases governed by lineardifferential equations, as given in the figure
Fig. A1. Hypothetical distributions of liquid, gas, and liquid-gasinterfaces for a simple system of vertical capillaries connected byhorizontal throats

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