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[vc_row][vc_column][vc_column_text] The occurrence and distribution of groundwater are controlled primarily by the geology of the area and the quantum of recharge received by the existing aquifer formations. Thus the alluvial

[vc_row][vc_column][vc_column_text] Water first enters an aquifer through gravity-induced downward movement (percolation), but it also flows in a lateral direction within an aquifer. This flow can occur due to the dip

[vc_row][vc_column][vc_column_text] Regionally, the top surface of the saturated zone is visualized as flat as the top of a table and hence this surface is referred to as the water table.

[vc_row][vc_column][vc_column_text] Sometimes they mean the same, but not always. While the uppermost level (top) of the saturated zone in an unconfined aquifer is the water table, the water level seen

[vc_row][vc_column][vc_column_text] Rainfall (precipitation), an integral part of the hydrological cycle, is the source of all fresh water on the earth. We tend to misjudge the enormous quantity of water brought

[vc_row][vc_column][vc_column_text] From the hydrogeology point of view, rock formations are categorized conveniently as unconsolidated (loose), consolidated (hard) and semi-consolidated. Recent and older alluviums are unconsolidated sedimentary formations, usually as alternate

[vc_row][vc_column][vc_column_text] Groundwater moves through porous rock formations, similar to water flowing through a sponge with interconnected pores. In nature, no space remains empty. Therefore, the pore space within the underground

[vc_row][vc_column][vc_column_text] Common methods of treating drinking water to remove/reduce the TDS and other harmful ions like Iron, Arsenic and Fluoride are Membrane separation Oxidation-flocculation-filtration Use absorbents such as activated alumina,