Determination of specific yield using a water balance approach - case study of Torla Odha watershed in the Deccan Trap province, Maharastra State, India

• Published in: Hydrogeology journal Vol. 14; no. 4; pp. 625 - 635
• Main Authors: Saha, Dipankar, Agrawal, A. K
• Format: Journal Article
• Language: English
• Published: Heidelberg Berlin/Heidelberg : Springer-Verlag 01.04.2006; Springer Nature B.V
• Subjects: Annual rainfall; Aquifer systems; Aquifers; Basalt; Deccan basalt; Dewatering; Dug wells; Geology; Groundwater; Groundwater levels; Groundwater management; groundwater recharge; Specific yield; Volumetric analysis; Water balance; Water demand; Water levels; Watersheds; India; India, Maharashtra, Ahmadnagar Dist., Bhima R
• ISSN: 1431-2174; 1435-0157
• DOI: 10.1007/s10040-005-0471-4

Specific yield is an essential parameter for any groundwater management plan. Volumetric analysis in the domain of groundwater budgeting for the non-monsoon months has been undertaken for a typical watershed of the Deccan basalt province. The Torla Odha watershed covers an area of over 22 km² on a third-order tributary of the westerly flowing Bhima River. The watershed receives a normal annual rainfall of 643 mm. The entire water demand is supplied by dug wells, which penetrate a shallow aquifer. The specific yield was estimated by comparing the monthly net volume of water removed from the aquifer, with the volume of aquifer de-saturated, based on monthly water level data. The estimated specific yield ranges from 0.0019 in May to 0.0173 in November with an average value of 0.0093. A correlation of the groundwater levels with the detailed geology suggests that the higher specific yield value (0.017) corresponds to dewatering of the weathered zone within the shallow aquifer. The specific yield of the massive basalt immediately below the weathered zone varies from 0.0089 to 0.0103. The underlying vesicular basalt, which is dissected by sheet joints, has a relatively higher specific yield (0.0121). The massive basalt, which forms the base of the shallow aquifer system, has a lower specific yield from 0.0019 to 0.0022.