A study on the correlation between soil radon potential and average indoor radon potential in Canadian cities

2017 ◽  
Vol 166 ◽  
pp. 152-156 ◽  
Author(s):  
Jing Chen ◽  
Ken L. Ford
2009 ◽  
Vol 136 (1) ◽  
pp. 56-60 ◽  
Author(s):  
J. Chen ◽  
R. Falcomer ◽  
L. Bergman ◽  
J. Wierdsma ◽  
J. Ly

2020 ◽  
Author(s):  
Meabh Hughes ◽  
Quentin Crowley

<p>Radon is a radioactive gas which emanates from rock, soil and water. Radon concentrations in the<br>atmosphere are generally very low (typically <5 Bq m-3), however it can occur at much higher levels<br>in soil (typically 10’s-100’s kBq m-3), or enclosed spaces such as buildings and caves (typically 10’s-<br>100’s Bq m-3). Exposure to radon and its daughter products is associated with an elevated risk of<br>developing lung cancer. Ireland has a population weighted indoor radon concentration of 98 Bq m-3<br>resulting in an estimated 300 annual lung cancer cases per year, representing approximately 12% of<br>the annual lung cancer cases. A national-scale legislative radon-risk map has a 10 x 10 km spatial<br>resolution and is based exclusively on indoor radon measurements (i.e. it does not contain any<br>geological information). The legislative map satisfies the European Council Directive<br>2013/59/EURATOM Basic Safety Standard, in that it defines “high radon” areas as those where >10%<br>of homes are estimated to exceed the national reference level of 200 Bq m-3. New buildings in such<br>areas are legally required to have a barrier, with low radon permeability installed.</p><p>This research focuses on a karstic region of SE Ireland, which features some exceptionally high<br>indoor radon concentrations (65,000 Bq m-3), even though it is not classified as a “high radon” area<br>on the national legislative map. Here we demonstrate the use of measuring sub-soil radon<br>concentrations and sub-soil permeability, in order to construct a radon potential (RP) map of the<br>area. Extremely high sub-soil radon concentrations (>1443 kBqm-3) and radon potential values<br>(>200) are spatially associated with Namurian shales, interbedded with limestone. Overall, we<br>classify the study area as high radon potential (RP >35) using this technique. We suggest all areas<br>underlain by Namurian shales in Ireland should undergo similar radon potential mapping, and if<br>necessary, should be re-designated as “high radon” areas. If deemed appropriate (i.e. where RP<br>>35), such a designation will help to protect the general public from the harmful effects of indoor<br>radon exposure, and will help to lower the incidence of radon-related lung cancer in these areas.</p>


Author(s):  
Jing Chen ◽  
Renato Falcomer ◽  
Lauren Bergman ◽  
Jessica Wierdsma ◽  
Jim Ly

Eos ◽  
2020 ◽  
Vol 101 ◽  
Author(s):  
Aaron Sidder

Researchers in Kentucky have merged results from home test kits with the state’s geologic map to produce a map of indoor radon potential based on the geology underlying homes in the state.


2019 ◽  
Vol 43 (5) ◽  
pp. 456-473
Author(s):  
Loren Gulabyants ◽  
Mihail Livshits ◽  
Alexandr Kalaydo ◽  
Konstantin Kovler

Two-dimensional model of the steady-state diffusion radon transport from the soil to the ground floor of the building is developed. Radon concentration distributions in the soil and the living space are calculated at different foundation geometries. The model considers radon entry from enclosing structures, outside air, and diffusion from the soil. The radon field under the building is described. The quantitative criteria for the resistance of the building foundation to radon penetration from the soil are defined. It is found that the resistance of the ground slab to radon penetration and radon concentration in the plane of the soil structure contact have a decisive influence on indoor radon, and that the initial distribution of radon concentration in the soil changes significantly after the building erection. These changes depend on the radon potential in the soil, its radon permeability, resistance of the floor structure to radon penetration, and building geometry.


1999 ◽  
Vol 21 (8) ◽  
pp. 723-731 ◽  
Author(s):  
Douglas G. Mose, George W. Mushrush
Keyword(s):  

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