Using geogenic radon potential to assess radon priority area designation, a case study around Castleisland, Co. Kerry, Ireland

• Main Authors: Banríon, M.H (Author), Crowley, Q.G (Author), Elío, J. (Author)
• Format: Article
• Language: English
• Published: Elsevier Ltd 2022
• Subjects: Case-studies; Gas permeability; Geogenic; Geogenic radon map; Geology; Indoor radon; Indoor radon measurements; Permeability measurements; Radon; Radon anomalies; Risk assessment; Smoke; Soil gas radon; Soil permeability; Soil surveys; Soil-gas concentrations; Soils
• Online Access: View Fulltext in Publisher

 Globally, indoor radon exposure is the leading cause of lung cancer in non-smokers and second most common cause after tobacco smoking. Soil-gas radon is the main contributor to indoor radon, but its spatial distribution is highly variable, which poses certain challenges for mapping and predicting radon anomalies. Measurement of indoor radon typically takes place over long periods of time (e.g. 3 months) and is seasonally adjusted to an annual average concentration. In this article we investigate the suitability of using soil-gas radon and soil-permeability measurements for rapid radon risk assessments at local scale. The area of Castleisland, Co. Kerry was chosen as a case study due to availability of indoor radon data and the presence of significant radon anomalies. In total, 135 soil-gas and permeability measurements were collected and complemented with 180 indoor radon measurements for an identical 6 km2 area. Both soil-gas and indoor radon concentrations ranged from very low (<10 kBqm−3, 0.1 Bqm−3) to anomalously high (>1433 kBqm−3, 65,000 Bqm−3) values. Our method classifies almost 50% of the area as a high radon potential area, and allows assessment of geogenic controls on radon distribution by including other geological variables. Cumulatively, the percentage of indoor radon variance explained by soil-gas radon concentration, bedrock geology, subsoil permeability and Quaternary geology is 34% (16%, 10%, 4% and 4% respectively). Soil-gas and indoor radon anomalies are associated with black shales, whereas the presence of karst and geological faults are other contributing factors. Sampling of radon soil-gas and soil permeability, used in conjunction with other geogenic data, can therefore facilitate rapid designation of radon priority areas. Such an approach demonstrates the usefulness of high-resolution geogenic maps in predicting indoor radon risk categories when compared to the application of indoor radon measurements alone. This method is particularly useful to assess radon potential in areas where indoor radon measurements are sparse or lacking, with particular application to rural areas, land rezoned for residential use, or for sites prior to building construction. © 2022 The Authors