Abstract:
Mewat district in Haryana located in the semi-arid region of India has been reported continual increase of
groundwater salinity. Stable isotopes, d18O and dD, of groundwater and rain water were successfully used
for characterization and source identiBcation of salinity aAected groundwater in the area. Eleven representative groundwater samples were of the pre-monsoon (May), monsoon (August) and post-monsoon
(November) seasons were analyzed for determining EC, d18O, dD and other parameters. The mean EC of
the samples was determined 6712 lS/cm for the pre-monsoon, 4743 lS/cm for the monsoon and 6602 lS/
cm for the post-monsoon. The slope of LMWL (8.13) obtained from the bivariate plot showed a very close
to the GMWL (8) and the slope of rain water (7.47) and groundwater samples found lied on the right of
the LMWL for all the seasons. Slopes observed for the pre-monsoon (6.76), monsoon (5.63) and postmonsoon (6.11) seasons indicated some evaporative enrichment of water before the groundwater recharge.
The increase of d-excess values from 0.74 in pre-monsoon to 3.75 in monsoon and 4.46 in post-monsoon
seasons suggested modern recharge with low evaporation. The recharge by meteoric water was noted from
the decrease in the mean value of EC in the monsoon season and its increase in the post-monsoon season,
which suggested possible ‘mechanism of mixing’. All these processes qualitatively predicted the recharge
and discharge locations in the study area.
