Table 1 Weightage of different classes for identification of groundwater prospect zone.
Parameters | Classes | Wi | Weight | Influence% | Rank |
---|---|---|---|---|---|
Rainfall | Low | 0.144 | 0.33 | 33 | 1 |
Moderate | 0.277 | 3 | |||
High | 0.579 | 4 | |||
CI – 0.005 | RI −0.58 | CR-0.008 | |||
Geology | Charnockite | 0.118 | 0.23 | 23 | 4 |
Hornblende biotite gneiss | 0.203 | 3 | |||
Epidote–hornblende gneiss | 0.162 | 1 | |||
Garnet-sillimanite gneiss | 0.071 | 2 | |||
Quartz vein | 0.035 | 1 | |||
Shales with bands of limestone | 0.344 | 3 | |||
Syenite/Nephelene syenite corrundun syenite | 0.065 | 2 | |||
CI – 0.010 | RI −1.32 | CR-0.008 | |||
Geomorphology units | Valley fill | 0.203 | 0.18 | 18 | 4 |
Denudational hills | 0.219 | 3 | |||
Structural hill | 0.098 | 1 | |||
Pediplain | 0.240 | 2 | |||
Piedmont zone | 0.240 | 2 | |||
CI – 0.115 | RI −1.12 | CR-0.008 | |||
Slope | Gentile slope | 0.099 | 0.8 | 8 | 3 |
Moderate slope | 0.210 | 2 | |||
Steep slope | 0.345 | 1 | |||
Very steep slope | 0.345 | 1 | |||
CI – 0.023 | RI – 0.026 | CR-0.009 | |||
Lineament density | Very high lineament density | 0.125 | 0.5 | 5 | 4 |
Moderate lineament density | 0.194 | 3 | |||
Low lineament density | 0.356 | 2 | |||
Very low lineament density | 0.325 | 1 | |||
CI – 0.016 | RI – 0.018 | CR-0.009 | |||
Drainage density | Very high drainage density | 0.130 | 0.7 | 7 | 1 |
Moderate drainage density | 0.159 | 2 | |||
Low drainage density | 0.296 | 3 | |||
Very low drainage density | 0.415 | 4 | |||
CI – 0.033 | RI – 0.036 | CR-0.009 | |||
Land use/land cover | Waterbody | 0.101 | 0.3 | 3 | 4 |
Cultivation land | 0.191 | 3 | |||
Forest lands | 0.258 | 3 | |||
Waste land rock surface | 0.294 | 1 | |||
Settlements | 0.156 | 1 | |||
CI – 0.068 | RI – 0.061 | CR-1.12 | |||
Soil | Alfisols | 0.169 | 0.3 | 3 | 2 |
Entisols | 0.092 | 2 | |||
Forest unsurveys | 0.160 | 3 | |||
Hill soil | 0.130 | 3 | |||
Inceptisols | 0.143 | 4 | |||
Reserve forest | 0.185 | 2 | |||
Water bodies | 0.120 | 4 | |||
CI – 0.123 | RI – 0.093 | CR-1.32 |