The 222Rn content of groundwater in strata of the Plio-Pleistocene Osaka Group in the Sennan area, Japan

Studies on the 222Rn content of groundwater were conducted to obtain knowledge of its distribution in the geosphere just below ground surface and below the depth of 100 m in the Osaka Group (Plio-Pleistocene). Samples analyzed from ten bore holes within 10 m depth below land surface showed that a sa...

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Published inJournal of hydrology (Amsterdam) Vol. 60; no. 1; pp. 197 - 207
Main Authors Fukui, M., Katsurayama, K.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 1983
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Abstract Studies on the 222Rn content of groundwater were conducted to obtain knowledge of its distribution in the geosphere just below ground surface and below the depth of 100 m in the Osaka Group (Plio-Pleistocene). Samples analyzed from ten bore holes within 10 m depth below land surface showed that a sandy layer contained groundwater with consistent radon concentrations except for a few locations where the variations in the water level were large due to precipitation and/or the water level was within 2 m of ground surface. The average 222Rn concentration in groundwater within 10 m of land surface was found to be approximately equal to 1 3 to 3 5 of the highest concentration found in groundwater from a well penetrating 100–200 m (420 pCi/l −1).
AbstractList Studies on the 222Rn content of groundwater were conducted to obtain knowledge of its distribution in the geosphere just below ground surface and below the depth of 100 m in the Osaka Group (Plio-Pleistocene). Samples analyzed from ten bore holes within 10 m depth below land surface showed that a sandy layer contained groundwater with consistent radon concentrations except for a few locations where the variations in the water level were large due to precipitation and/or the water level was within 2 m of ground surface. The average 222Rn concentration in groundwater within 10 m of land surface was found to be approximately equal to 1 3 to 3 5 of the highest concentration found in groundwater from a well penetrating 100–200 m (420 pCi/l −1).
Author Fukui, M.
Katsurayama, K.
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Cites_doi 10.1029/JB082i008p01353
10.3769/radioisotopes.13.5_362
10.1097/00004032-197610000-00005
10.1029/WR009i004p00885
10.1038/271516a0
10.1097/00004032-197806000-00015
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