Sub-surface investigations on deep saline groundwater of Charnockite rock formation, Kalpakkam, India.

Investigations on geohydrological aspects of coastal aquifer are important in order to understand the mechanism of ground water salinisation. The present study describes the salinity variations of ground water in deep boreholes drilled in Charnockite rock formation of Kalpakkam, on the eastern coast of India. Water samples collected up to 600m depth were analyzed for salinity variation. It is noticed that in one of the boreholes, (borehole K1), the salinity level is found to be 74 parts per thousand (ppt) at 400 m depth. Influence of surface saline water bodies viz., sea (26-28.5 ppt), backwaters (27-30 pt) and Buckingham canal (27-32 ppt) as the possible sources of recharge of fresh waters through joint and fracture system of the rock are discussed in this paper. Studies would assist in understanding the geohydrological characteristics of deep geological formation.

Experimental methodology to assess contaminant diffusion in rock mass.

Monitoring changes in electrical conductivity (EC) of aqueous phase, due to contaminant diffusion through porous media, is one of the techniques followed by researchers to understand the migration mechanism. However, the contaminant diffusion in the rock mass is a slow process and hence detecting small changes in conductivity with the help of conventional laboratory conductivity meters is quite difficult. With this in view, an experimental methodology to monitor diffusion of contaminant(s) through the intact and fractured rock mass, with the help of a USDTS (Ultra-Sensitive Devices and Technical Services) conductivity meter, has been developed. Results have been validated with those obtained from the ion chromatograph (IC) technique and a good agreement has been noted. The study demonstrates usefulness of the proposed methodology for online monitoring of contaminant migration through the porous media.