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On the coupled unsaturated–saturated flow process induced by vertical, horizontal, and slant wells in unconfined aquifers

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Figure

Figure 1. The schematic diagram of groundwater flow to a horizontal well (a) and a slant well (b) in an unsaturated–saturated system.
Fig. 2a and b, respectively. We also compare our solution tothe ZZ solution (unconfined aquifer) and the ZWP solution(confined aquifer)
Figure 2. (a) The log–log plot of(confined aquifer), and the sID against tD/r2D for different values of the dimensionless unsaturated parameter κD, the ZWP solution ZZ solution (unconfined aquifer)
Figure 3. The log–log plot of sID against tD/r2D for different angles of the well screen and a comparison with the ZZ solution for (a) dimen-sionless piezometer location (0, 0.05, and 0.9) and (b) dimensionless piezometer location (0, 0.05, and 0.1.)
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