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- W4382045440 abstract "The radiogenic isotope radon (222Rn) is an excellent tracer for monitoring and identifying several hydrogeological processes because of having a short half-life and considerably presence of large concentration in groundwater relative to the surface water. The groundwater radon distribution in various geological formation of coastal and inland regime in Kasaragod district was carried out using a RAD7 detector and RAD H2O accessory to determine the correlation amongst the geology of the study area and radon concentrations of groundwater. The study area is classified into five lithological groups that differ in groundwater occurrence in space and time. About 70 measurements of 222Rn from monitored open wells in the study area were analyzed. The 222Rn of the coastal alluvium region is ranged from 77.1 to 832 Bq/m3 and average radon concentration of 408 Bq/m3. In fluvial alluvium region, it is ranged from 39.6 to 479 Bq/m3 and average radon concentration of 440 Bq/m3. Gneiss /Khondalite/ Charnockite region is ranged from 117.5 to 2343 Bq/m3 and average radon concentration of 782 Bq/m3. In laterite region is ranged from 436 to 1114 Bq/m3 and average radon concentration of 636 Bq/m3 and in tertiary alluvium region, it is ranged from 37.8 to 1135 Bq/m3 and average concentration of 346 Bq/m3. High radon actions were primarily found in Gneiss /Khondalite /Charnockite rocks and Lateritic regions. Radon values were compared with the maximum contaminant levels (MCL) for potable water range good for human consumption proposed by USEPA which is 11.3 Bq L−1 and WHO is 100 Bq L−1and it was determined that the groundwater radon concentration values were well within the safe limit." @default.
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- W4382045440 date "2023-01-01" @default.
- W4382045440 modified "2023-09-23" @default.
- W4382045440 title "Emanation of Radon from Coastal and Inland Groundwater of Northern Kerala, India" @default.
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- W4382045440 doi "https://doi.org/10.1007/978-981-19-9151-6_41" @default.
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