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Fig. 12. (a) Matric pressures at 30-cm depth in the sampling, 
a, and natural, b, profiles, (b) cumulative precipitation and sampling amount, (c) 30-d averaged precipitation rate, sampling rate, and change in soil water storage from 0 to 30 cm deep in the sampling profile, 
S, (d) 30-d averaged loss rate due to evapotranspiration, ET, evaporation rate measured by small and large water-filled pans, Epan, and ET rate estimated by the Thornthwaite method, ETthorn, and (e) 30-d averaged soil water storage throughout the continuous-sampling period.
