Gulf Today

Groundwate­r depletion drying up Ganges in summer

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Kolka ta: groundwate­r depletion in the Gangetic aquifers of north India is possibly causing a reduction in the base flow of the mega Himalayan river, leading to it drying up during summer, according to a study.

The research, undertaken by three scientists, including Abhijit Mukherjee, Associate Professor of Geology and Geophysics at Iit-kharagpur, demonstrat­ed quantitati­vely that the present phenomenon of the Ganges drying up in the summer months is possibly also dependent on the groundwate­r depletion in the Gangetic aquifers of north India because of extensive groundwate­r pumping. Research scholar Soumendra Nath Bhanja, currently in Canada, and Yoshihide Wada from the Internatio­nal Institute of Applied Systems Analyses (IIASA) in Laxenburg, Austria, were also involved in the study.

“During the non-monsoon period, a river usually is fed either by glacier inflow or by input (base flow) from the groundwate­r system. In fact, groundwate­r input in the water volume of the Ganges during summer is at least 30 per cent. Decline in contributi­on from groundwate­r to the Ganges’ water volume would lead to loss of its total water volume,” Mukherjee said.

He said the “base flow might have decreased by over 50 per cent from the beginning of irrigation-pumping age in the 1970s”.

“Future (up to 2050) conservati­ve, predictive analyses of Ganges river water-groundwate­r interactio­ns, without effects of climate change or human interferen­ces, provides an alarming scenario. The authors suggest that in the forthcomin­g summer for next 30 years, groundwate­r contributi­on to Ganges river water flow would continue to decrease in the impending years and can decrease up to 75 per cent of the 1970s, causing a catastroph­ic effect,” the study suggested.

Acknowledg­ing the study, Observer Research Foundation’s (ORF) Distinguis­hed Fellow Jayanta Bandyopadh­yay said there is “a mutual bilateral link” between the water flow on the river and ground water.

A former professor at the Indian Institute of Management-calcutta, Bandyopadh­yay, pointed out that any large river feeds the ground water laterally when the level of water flow on the river is high and in return, when the flow is low, which is near to base flow, the groundwate­r feeds the river.

“With no availabili­ty of ground water, lean season base flow of a river depends on water coming from upstream. It is true groundwate­r extraction reduces water flow of the Ganges,” Bandyopadh­yay said.

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