Estimation of groundwater recharge from water storage structures in a semi-arid climate of India

• Published in: Journal of hydrology (Amsterdam) Vol. 329; no. 1; pp. 224 - 243
• Main Authors: Sharda, V.N., Kurothe, R.S., Sena, D.R., Pande, V.C., Tiwari, S.P.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 30-09-2006; Elsevier Science
• Subjects: Chloride mass balance; Earth sciences; Earth, ocean, space; Exact sciences and technology; Hydrology. Hydrogeology; Potential recharge; Recharge function; Water storage structures; Water table fluctuation; India; Water table fluctuation; Potential recharge; Water storage structures; Recharge function; Chloride mass balance; chlorides; rainfall; mass balance; water table; ground-water recharge; concentration; exhibits; climate; halides; depth; water storage; Asia; fluctuations; annual average
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2006.02.015

Groundwater recharge from water storage structures under semi-arid conditions of western India has been estimated by employing water table fluctuation (WTF) and chloride mass balance (CMB) methods. Groundwater recharge was estimated as 7.3% and 9.7% of the annual rainfall by WTF method for the years 2003 and 2004, respectively while the two years average recharge was estimated as 7.5% using CMB method. A Recharge function depicting the relationship between potential recharge from storage structures and successive day averaged storage depths was better exhibited by a power function. A diagnostic relationship correlating the rainfall to the potential recharge from water storage structures has been developed to explain the characteristics of the storage structures for a given geographical location. The study has revealed that a minimum of 104.3
mm cumulative rainfall is required to generate 1
mm of recharge from the water storage structures. It was also inferred that the storage structures have limited capacity to induce maximum recharge irrespective of the amount of rainfall and maximum recharge to rainfall ratio is achieved at a lower rainfall than the average annual rainfall of the area. An empirical linear relationship was found to reasonably correlate the changes in chloride concentration with water table rise or fall in the study area.