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http://dx.doi.org/10.9720/kseg.2012.4.427

Hydrochemistry and Distribution of Uranium and Radon in Groundwater of the Nonsan Area  

Cho, Byeong Wook (Groundwater Department, Korea Institute of Geoscience and Mineral Resources)
Kim, Moon Su (Soil and Groundwater Research Division, National Institute of Environmental Research)
Kim, Tae Seung (Soil and Groundwater Research Division, National Institute of Environmental Research)
Han, Jin Seok (Soil and Groundwater Research Division, National Institute of Environmental Research)
Yun, Uk (Groundwater Department, Korea Institute of Geoscience and Mineral Resources)
Lee, Byeong Dae (Groundwater Department, Korea Institute of Geoscience and Mineral Resources)
Hwang, Jae Hong (Geological Research Division, Korea Institute of Geoscience and Mineral Resources)
Choo, Chang Oh (Department of Geology, Kyungpook National University)
Publication Information
The Journal of Engineering Geology / v.22, no.4, 2012 , pp. 427-437 More about this Journal
Abstract
A total of 100 groundwater samples were collected from the Nonsan area and the behaviors of uranium and radon as natural radionuclides were investigated with respect to other physicochemical components in the groundwater in order to understand their occurrence, properties, and origins. Radionuclide levels were used to construct detailed concentration maps. The concentration of uranium ranges from 0 to 378 ${\mu}g/L$, with an average of 8.57 ${\mu}g/L$, standard deviation of 42.88 ${\mu}g/L$, and median of 0.56 ${\mu}g/L$. The correlation coefficient between uranium and radon is 0.42, whereas these radionuclides show no relation with other physicochemical components in groundwater. It is noteworthy that the uranium level in most samples (97% of the samples) is less than 30 ${\mu}g/L$, where the bedrock of the aquifer is granite or complex rocks located along the boundary between granite and metamorphic rocks. In the Okcheon metamorphic belt, the uranium concentration of most groundwater is less than 1 ${\mu}g/L$. Radon levels varies from 128 to 9,140 pCi/L, with an average of 2,186 pCi/L, standard deviation of 1,725 pCi/L, and median of 1,805 pCi/L. High radon levels (> 4,000 pCi/L) are most common in regions of Jurassic granite, whereas low radon areas are found in regions of sedimentary rock. In conclusion, the distribution and occurrence of radionuclides are intimately related to the basic geological characteristics of the rocks in which the radiogenic minerals are primarily contained.
Keywords
Nonsan area; Uranium; Radon; Groundwater; Detailed concentration maps;
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Times Cited By KSCI : 5  (Citation Analysis)
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