Ground Water Studies

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Hydrological cycle
Most water on our planet occurs as saline water in the oceans and deep underground or is contained in polar ice caps and the permanent ice cover of the high mountain ranges. So, only 30 million km3 of fresh water, which is only 2 percent of all water, plays an active part in the hydrological cycle and in the maintenance of all life on the continents. The hydrological cycle depicts how part of the ocean water evaporates, the water vapor turns into freshwater precipitation (rain, hail, snow) on the earth’s surface (seas, land), then flows over the land surface (glaciers, runoff, streams) and partly infiltrates into the soil (soil water) to be used by the vegetation (evapotranspiration) or to recharge the groundwater bodies. Subsequently, most groundwater returns either by being pumped or by natural outflow, to surface water bodies which subsequently discharge back into the sea.

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