Understanding groundwater systems and their functioning through the study of stable water isotopes in a hard-rock aquifer (Maheshwaram watershed, India)

SummaryGroundwater degradation through abstraction, contamination, etc., shows a world-wide increase and has been of growing concern for the past decades. In this light, the stable isotopes of the water molecule (δ18O and δ2H) from a hard-rock aquifer in the Maheshwaram watershed (Andhra Pradesh, India) were studied. This small watershed (53 km2) underlain by granite, is endorheic and representative of agricultural land-use in India, with more than 700 bore wells in use. In such a watershed, the effect of overpumping can be severe and the environmental effects of water abstraction and contamination are of vital importance. A detailed and dynamic understanding of groundwater sources and flow paths in this watershed thus is a major issue for both researchers and water managers, especially with regards to water quality as well as the delimitation of resources and long-term sustainability.To this end, the input from monsoon-precipitation was monitored over two cycles, as well as measuring spatial and temporal variations in δ18O and δ2H in the groundwater and in precipitation. Individual recharge from the two monsoon periods was identified, leading to identification of periods during which evaporation affects groundwater quality through a higher concentration of salts and stable isotopes in the return flow. Such evaporation is further affected by land-use, rice paddies having the strongest evapotranspiration.

Research highlights
► Stable-isotopes from hard-rock aquifer in India defined a dynamic pictures.
► Stable isotopes in monsoon cycles allowed defining two geographical monsoon signals.
► The recharge isotopic signature in the watershed fluctuates between the two monsoons.
► Individual open-end wells shows a different functioning depending on recharge and use.