SPATIAL ASSOCIATION BETWEEN RESIDENTIAL RADON CONCENTRATION AND BEDROCK TYPES IN NEW HAMPSHIRE

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dc.contributor.author Shi X.
dc.contributor.author Hoftiezer D.J.
dc.contributor.author Duell E.J.
dc.contributor.author Onega T.L.
dc.date.accessioned 2024-09-20T06:16:47Z
dc.date.available 2024-09-20T06:16:47Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=52817834
dc.identifier.citation Environmental Geology, 2006, 51, 1, 65-71
dc.identifier.issn 0943-0105
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/45220
dc.description.abstract Using a large database of residential short-term radon measurements in New Hampshire, this study evaluated the ability of expert-assigned bedrock radon potential for predicting residential radon concentration. First, each bedrock type was assigned a radon potential level by a geologist familiar with the local geology. Then, using residential radon measurements, a continuous surface of radon concentration was generated through a kriging process. The mean residential radon concentration within the spatial extent of each bedrock type was then calculated based on that surface. The Spearman Rank Correlation Coefficient was calculated between the two ranks of the bedrock types, one based on the expert-assigned potential level and the other based on the mean residential concentration. A strong correlation between the rank correlation and the area of the bedrock type was found. When only the 15 largest bedrock types were used, the Spearman Correlation Coefficient reached 0.6. Geological knowledge is concluded to be useful in predicting and mapping residential radon concentration, but the prediction should be interpreted with caution, especially for areas in which the underlying bedrocks are highly localized.
dc.subject BEDROCK
dc.subject RESIDENTIAL RADON
dc.subject KRIGING
dc.subject SPEARMAN CORRELATION
dc.subject NEW HAMPSHIRE
dc.title SPATIAL ASSOCIATION BETWEEN RESIDENTIAL RADON CONCENTRATION AND BEDROCK TYPES IN NEW HAMPSHIRE
dc.type Статья
dc.identifier.doi 10.1007/s00254-006-0304-3


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