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The diagram indicates that Ca Mg HCO3 is the major water type dominant in pre-monsoon and Ca HCO3 is the major water type dominant in post-monsoon.
The former happens to be fresh water and the major water type in the study area.
The groundwater samples fall in three of major water type fields representing (1) Ca–Mg–HCO3, (2) CandO4 and (3) Na Cl facies.
The major water type identified in the area is the Na HCO3 and occupies about 63%% of the water samples in the study area.
Figure 7 shows that the dominant cations and anions were (Na+ + K+) and Cl−, respectively and the major water type was Na Cl followed by mixed CaMgCl and CaHCO3 in that order.
The dominant water facies in the lake is Mg-SO4, however, the subdivision of diamond shape in piper trilinear diagram suggests the major water type followed by Mg-SO4 is Ca-Cl2 type.
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The Chadha diagram (Chadha 1999) was used to define the major water types in the areas.
Cluster analysis in Q-mode resulted in three major water types (HCO3− Ca-2+dominated, Cl− HCO3− Ca2+-dominated and Cl− HCO3− Ca2+-dominatedfor the groundwandr.
Piper trilinear diagram (Piper 1953) suggests that there are two major water types, mainly Ca Na HCO3 and mixed Ca Mg Cl prevailing in the groundwater environment (Fig. 3).
The major water types present are Na Mg Cl, Na Mg HCO3 and Mg Na(Ca)–HCO3 in the pre-monsoon and Na Mg Cl, Ca Mg HCO3 and Mg Ca HCO3 in the post-monsoon.
The major water cycle type is characterized by non-changing precipitation and increasing evapotranspiration (PNO-EIN), which covers 20.88% of globally land.
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