HIGHLIGHTS
SUMMARY
A precise mapping of groundwater recharge potential zones in typical basins might help with resourceful management of this critical source and reduce regional groundwater vulnerability. The fuzzy membership value created by map combination was used to divide the final groundwater recharge map into groups. One of the factors considered in groundwater recharge study was drainage density, and the cross-tabulation outcomes with groundwater recharge locations are displayed in Table 10. In contrast, majority of low drainage density areas (0-0.26 km/sq.km) were home for very high and high groundwater recharge potential . . .
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