Bossew P
German Federal Office for Radiation Protection, Köpenicker Allee 120-130, 10318 Berlin, Germany.
J Environ Radioact. 2015 Mar;141:44-50. doi: 10.1016/j.jenvrad.2014.11.020. Epub 2014 Dec 17.
A radon prone geology is one for which the probability is increased that in a house built on it, elevated indoor Rn concentration will be encountered, or that its Rn potential will be increased. Labelling geological units as Rn prone or not can be an important support in deciding whether a geographical or administrative region in which that geological unit occurs, should be called Rn prone area, possibly in absence of other predictors. In this article a method is proposed which, given a set of geological classes, sorts the classes into Rn prone and non-Rn prone classes depending on a classification criterion which one can choose according the purpose. The method is computationally simple and is demonstrated on the example of Germany.
氡易生地质是指在其上建造房屋时，室内氡浓度升高或其氡潜能增加的概率增大的地质。将地质单元标记为氡易生或不易生，对于决定某个地质单元所在的地理或行政区是否应被称为氡易生地区可能具有重要的支持作用，特别是在缺乏其他预测指标的情况下。本文提出了一种方法，给定一组地质类别，根据可根据目的选择的分类标准，将这些类别分为氡易生类别和非氡易生类别。该方法计算简单，并以德国为例进行了演示。
