Abstract
In Neyveli, Tamilnadu, India, a deep-seated multi-layered confined aquifer is being continuously pumped to permit safe mining of lignite. This paper highlights the various ground water recharge studies undertaken to quantify the potential of recharging the Neyveli hydrogeological basin to maintain the regional ground water balance. GIS studies were used to analyze artificial recharge in the Neyveli basin, commencing from the deep water table zone (recharge area) in the western upland part, the confined aquifer zone closer to the active mining area, and the confined zone further away in the east, down-dip and closer to the coast.
Sign-in/Register to access full text options 
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 callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
