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Measurements of radon concentrations in groundwaters from Swaziland using CR-39 nuclear track detectors
Several studies have shown that water-borne 222Rn contributes to indoor air concentrations. A passive radon measurement method was employed to determine radon activity concentrations in groundwater in wells of Swaziland. Concentrations ranged between 1.8 ± 0.1 and 152.9 ± 4.8 Bq L −1, with only slig...
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Published in: | Applied radiation and isotopes 1996, Vol.47 (3), p.383-385 |
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container_title | Applied radiation and isotopes |
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creator | Farid, S.M. |
description | Several studies have shown that water-borne
222Rn contributes to indoor air concentrations. A passive radon measurement method was employed to determine radon activity concentrations in groundwater in wells of Swaziland. Concentrations ranged between 1.8 ± 0.1 and 152.9 ± 4.8 Bq L
−1, with only slight variations (maximum 2.4σ from the mean) over 1 yr in a typical well. The arithmetic mean
222Rn concentration measured in groundwater supplies was 25.2 Bq L
−1; geometric mean 13.5 Bq L
−1. Fifty-four percent of the wells had
222Rn water concentrations in excess of the U.S. Environmental Protection Agency's proposed limit of 11 Bq L
−1 (300 pCi L
−1) for public drinking water supplies. |
doi_str_mv | 10.1016/0969-8043(95)00284-7 |
format | article |
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222Rn contributes to indoor air concentrations. A passive radon measurement method was employed to determine radon activity concentrations in groundwater in wells of Swaziland. Concentrations ranged between 1.8 ± 0.1 and 152.9 ± 4.8 Bq L
−1, with only slight variations (maximum 2.4σ from the mean) over 1 yr in a typical well. The arithmetic mean
222Rn concentration measured in groundwater supplies was 25.2 Bq L
−1; geometric mean 13.5 Bq L
−1. Fifty-four percent of the wells had
222Rn water concentrations in excess of the U.S. Environmental Protection Agency's proposed limit of 11 Bq L
−1 (300 pCi L
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222Rn contributes to indoor air concentrations. A passive radon measurement method was employed to determine radon activity concentrations in groundwater in wells of Swaziland. Concentrations ranged between 1.8 ± 0.1 and 152.9 ± 4.8 Bq L
−1, with only slight variations (maximum 2.4σ from the mean) over 1 yr in a typical well. The arithmetic mean
222Rn concentration measured in groundwater supplies was 25.2 Bq L
−1; geometric mean 13.5 Bq L
−1. Fifty-four percent of the wells had
222Rn water concentrations in excess of the U.S. Environmental Protection Agency's proposed limit of 11 Bq L
−1 (300 pCi L
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222Rn contributes to indoor air concentrations. A passive radon measurement method was employed to determine radon activity concentrations in groundwater in wells of Swaziland. Concentrations ranged between 1.8 ± 0.1 and 152.9 ± 4.8 Bq L
−1, with only slight variations (maximum 2.4σ from the mean) over 1 yr in a typical well. The arithmetic mean
222Rn concentration measured in groundwater supplies was 25.2 Bq L
−1; geometric mean 13.5 Bq L
−1. Fifty-four percent of the wells had
222Rn water concentrations in excess of the U.S. Environmental Protection Agency's proposed limit of 11 Bq L
−1 (300 pCi L
−1) for public drinking water supplies.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/0969-8043(95)00284-7</doi><tpages>3</tpages></addata></record> |
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title | Measurements of radon concentrations in groundwaters from Swaziland using CR-39 nuclear track detectors |
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