Estimating aquifer properties and distributed groundwater recharge in a hard-rock catchment of Udaipur, India

Abstract

The present study determined aquifer parameters in hard - rock aquifer system of Ahar River catchment, Udaipur, India by conducting 19 pumping tests in largediameter wells. Spreadsheet programs were developed for analyzing pumping test data, and their accuracy was evaluated by root mean square error (RMSE) and correlation coefficient (R). Histograms and Shapiro - Wilk test indicated non - normality (p value \ 0.01) of pre - and postmonsoon groundwater levels at 50 sites for years 2006 - 2008, and hence, logarithmic transformations were done. Furthermore, recharge was estimated using GISbased water table fluctuation method. The groundwater levels were found to be influenced by the topography, presence of structural hills, density of pumping wells, and seasonal recharge. The results of the pumping tests revealed that the transmissivity (T) ranges from 68 - 2239 m2 / day, and the specific yield (Sy) varies from 0.211 to 0.51 9 10 - 5 . The T and Sy values were found reasonable for the hard - rock formations in the area, and the spreadsheet programs were found reliable (RMSE) *0.017 - 0.339 m; R[0.95]. Distribution of the aquifer parameters and recharge indicated that the northern portion with high ground elevations (575 - 700 m MSL), and high Sy (0.08 - 0.25) and T (600 m2 / day) values may act as recharge zone. The T and Sy values revealed significant spatial variability, which suggests strong heterogeneity of the hard - rock aquifer system. Overall, the findings of this study are useful to formulate appropriate strategies for managing water resources in the area. Also, the developed spreadsheet programs may be used to analyze the pumping test data of large - diameter wells in other hard - rock regions of the world.