Abstract

The present study determined aquifer parameters in hard-rock aquifer system of Ahar River catchment, Udaipur, India by conducting 19 pumping tests in large-diameter 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 post-monsoon groundwater levels at 50 sites for years 2006–2008, and hence, logarithmic transformations were done. Furthermore, recharge was estimated using GIS-based 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 × 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.

Highlights

  • Estimating hydraulic characteristics of aquifer systems is an essential part of groundwater studies

  • Spreadsheet programs were developed for analyzing pumping test data, and their accuracy was evaluated by root mean square error (RMSE) and correlation coefficient (R)

  • This study explored the effect of the rainfall occurrence on the groundwater level fluctuation by plotting bar charts of Interpolating groundwater levels by geostatistical modeling and geographical information system (GIS) technique

Read more

Summary

Introduction

Estimating hydraulic characteristics (transmissivity and storage coefficient or specific yield) of aquifer systems is an essential part of groundwater studies. The most effective, reliable and standard way of determining these characteristics is to conduct and analyze hydraulic tests such as pumping test. When the pumping tests are performed in small-diameter wells, several methods are available for analyzing the pumping test data (Theis 1935; Cooper and Jacob 1946; Neuman 1974; Hantush 1964) depending upon the type of aquifer. These methods are based on one of the assumptions that pumping test is performed in small-diameter well for which storage can be neglected. At later stages of time, almost entire pumped water is supplied from the aquifer (Rushton 2003)

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call