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Table 1 Aquifer parameters evaluated in dug wells Well no.
Gibbs diagram reflected evaporation as a dominant phenomenon in dug well; however, tube well samples are declined toward rock dominance.
In contrast, the average (Na+ + K+)/TZ+ ratio was slightly higher than that of (Ca2+ + Mg2+)/TZ+ in dug wells.
The high coefficients of variance (CV > 50%; Table 2) and spatial distribution, illustrated by boxplots (Fig. 3), showed a heterogeneous abundance of most physicochemical parameters in dug wells.
Average composition on stiff diagram signifies supremacy of Na Cl along with Mg SO4 as second dominant pair in dug well samples (Fig. 2).
This is consistent with the low K+ (except W5 and B4) concentrations in dug well and borewell waters relative to tap waters (8 11 mg/L).
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