Abstract
The study investigates the spatio-temporal variability of radon (222Rn) with respect to the geology and hydrogeology of the Vamanapuram River Basin (VRB), SW India. A total of 40 groundwater samples were collected during three seasons of 2019. RAD7, RAD-H2O accessory (Durridge Co. USA) was used to analyse 222Rn, and physico-chemical parameters were measured in situ by Horiba Laqua water quality analyser. The results show that the 222Rn activity was in the range of 640–79,940 Bq/m3 in pre-monsoon, 250–36,950 Bq/m3 in monsoon and 420–59,790 Bq/m3 in post-monsoon season and 18% of samples exceeded the permissible limit of USEPA (11,000 Bq/m3) during all seasons. Remarkably, the samples exceeding the permissible limit of 222Rn were associated with khondalitic rocks with notable amount of uranium-bearing minerals and NW-SE trending lineaments, the most active type of lineament in the study area. The study shows the considerable influence of seasons and the highest activities were found during pre-monsoon compared to the other two seasons.
Acknowledgments
The authors thankfully acknowledge Department of Science and Technology (DST) for providing financial assistance under DST-INSPIRE Fellowship for the successful completion of research work. The authors grateful to Central Groundwater Board (CGWB), Kerala region for providing lithology data which helps to interpret the results.
Disclosure statement
The authors declare that they have no known competing financial interest or personal relationships that could have appeared to influence the work reported in this paper.
Ethics approval statement
The manuscript has not been published in any other journal. The manuscript includes original data, acquired during our own research, and is not under consideration for publication elsewhere.