Geology Reference
In-Depth Information
10 hydraulic drawdown curves. These curves are summed up into two curves,
an average and a deviation curve respectively that can be compared to those
derived from the
in situ
measurements. The first point is try to simulate the
spatial variability of the responses, and then try to match the average
behaviour. Hereafter (Figs 3 and 4), we show some of satisfactory results
obtained using the parameters listed in Table 2. Obviously there is no unique
solution to the problem and we only suggest set of values that produce an
acceptable fit to the data, qualitatively and quantitatively.
Figure 3.
Calibration test, case 4.
Figure 4.
Calibration test, case 5.
