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Effect of unrepresented model errors on estimated soil hydraulic material properties

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Figure

Figure 1. View of ASSESS site with tensiometer access tube,weather station, and groundwater well along the left boundary
Figure 3. The position of the groundwater table was measured manually in the groundwater well and automatically with the tensiometer(Fig
Figure 4. The measured water content data for the three different phases (initial drainage, multistep imbibition, and multistep drainage –separated by the solid vertical black lines in the figure) show a high variability up to and beyond the validity limits
Table 2. During the experiment, ASSESS was forced with a fluctuating groundwater table
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