Abstract
The results reveal that the water-chemistry of Nalas and Rivers is superior to that of the Tals on account of their cations, anions and other properties. The calcium ions dominate within anions and bicarbonates within anions in all the waters irrespective of their sources and locations. Calcium and magnesium ions show a close resemblance in their concentration but sodium ions exhibit an erratic variation. Seasons too play a vital role on chemical characteristics/composition of the waters. The paper concludes with some suggestions.
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