Dataset Information

A Geologically Based Indoor-Radon Potential Map of Kentucky.

ABSTRACT: We combined 71,930 short-term (median duration 4 days) home radon test results with 1:24,000-scale bedrock geologic map coverage of Kentucky to produce a statewide geologically based indoor-radon potential map. The test results were positively skewed with a mean of 266 Bq/m³, median of 122 Bq/m³, and 75th percentile of 289 Bq/m³. We identified 106 formations with ?10 test results. Analysis of results from 20 predominantly monolithologic formations showed indoor-radon concentrations to be positively skewed on a formation-by-formation basis, with a proportional relationship between sample means and standard deviations. Limestone (median 170 Bq/m³) and dolostone (median 130 Bq/m³) tended to have higher indoor-radon concentrations than siltstones and sandstones (median 67 Bq/m³) or unlithified surficial deposits (median 63 Bq/m³). Individual shales had median values ranging from 67 to 189 Bq/m³; the median value for all shale values was 85 Bq/m³. Percentages of values falling above the U.S. Environmental Protection Agency (EPA) action level of 148 Bq/m³ were sandstone and siltstone: 24%, unlithified clastic: 21%, dolostone: 46%, limestone: 55%, and shale: 34%. Mississippian limestones, Ordovician limestones, and Devonian black shales had the highest indoor-radon potential values in Kentucky. Indoor-radon test mean values for the selected formations were also weakly, but statistically significantly, correlated with mean aeroradiometric uranium concentrations. To produce a map useful to nonspecialists, we classified each of the 106 formations into five radon-geologic classes on the basis of their 75th percentile radon concentrations. The statewide map is freely available through an interactive internet map service.

SUBMITTER: Haneberg WC

PROVIDER: S-EPMC7682569 | biostudies-literature | 2020 Nov

REPOSITORIES: biostudies-literature

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A Geologically Based Indoor-Radon Potential Map of Kentucky.

Haneberg William C WC Wiggins Amanda A Curl Douglas C DC Greb Stephen F SF Andrews William M WM Rademacher Kathy K Rayens Mary Kay MK Hahn Ellen J EJ

GeoHealth 20201101 11

We combined 71,930 short-term (median duration 4 days) home radon test results with 1:24,000-scale bedrock geologic map coverage of Kentucky to produce a statewide geologically based indoor-radon potential map. The test results were positively skewed with a mean of 266 Bq/m3, median of 122 Bq/m3, and 75th percentile of 289 Bq/m3. We identified 106 formations with ≥10 test results. Analysis of results from 20 predominantly monolithologic formations showed indoor-r ...[more]

PMID: 33283125

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Project description:Radon is the second-leading cause of lung cancer worldwide. Most indoor exposure occurs by diffusion of soil gas. Radon is also found in well water, natural gas, and ambient air. Pennsylvania has high indoor radon concentrations; buildings are often tested during real estate transactions, with results reported to the Department of Environmental Protection (PADEP).We evaluated predictors of indoor radon concentrations.Using first-floor and basement indoor radon results reported to the PADEP between 1987 and 2013, we evaluated associations of radon concentrations (natural log transformed) with geology, water source, building characteristics, season, weather, community socioeconomic status, community type, and unconventional natural gas development measures based on drilled and producing wells.Primary analysis included 866,735 first measurements by building, with the large majority from homes. The geologic rock layer on which the building sat was strongly associated with radon concentration (e.g., Axemann Formation, median = 365 Bq/m3, IQR = 167-679 vs. Stockton Formation, median = 93 Bq/m3, IQR = 52-178). In adjusted analysis, buildings using well water had 21% higher concentrations (? = 0.191, 95% CI: 0.184, 0.198). Buildings in cities (vs. townships) had lower concentrations (? = -0.323, 95% CI: -0.333, -0.314). When we included multiple tests per building, concentrations declined with repeated measurements over time. Between 2005 and 2013, 7,469 unconventional wells were drilled in Pennsylvania. Basement radon concentrations fluctuated between 1987 and 2003, but began an upward trend from 2004 to 2012 in all county categories (p < 0.001), with higher levels in counties having ? 100 drilled wells versus counties with none, and with highest levels in the Reading Prong.Geologic unit, well water, community, weather, and unconventional natural gas development were associated with indoor radon concentrations. Future studies should include direct environmental measurement of radon, as well as building features unavailable for this analysis.Casey JA, Ogburn EL, Rasmussen SG, Irving JK, Pollak J, Locke PA, Schwartz BS. 2015. Predictors of indoor radon concentrations in Pennsylvania, 1989-2013. Environ Health Perspect 123:1130-1137; http://dx.doi.org/10.1289/ehp.1409014.

Dataset Information

A Geologically Based Indoor-Radon Potential Map of Kentucky.

Publications

A Geologically Based Indoor-Radon Potential Map of Kentucky.

Similar Datasets

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