radon risk mapping
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2014 ◽  
Vol 29 (suppl.) ◽  
pp. 59-63 ◽  
Author(s):  
Francois Tondeur ◽  
Giorgia Cinelli

A computer code dedicated to indoor radon risk mapping is presented, based on geology and on indoor radon measurements. Assuming a lognormal distribution of the data at the local scale, it provides the estimation of the percentage of houses above a chosen reference level, at the points of a grid specified by the user, using the moving average of data belonging to the same geological unit as the grid point.


1994 ◽  
Vol 56 (1-4) ◽  
pp. 221-224 ◽  
Author(s):  
F. Kullman

Abstract The Swedish stipulations of a maximum radon daughter level of 200 Bq.m3 for permanently inhabited buildings, and of 70 Bq.m-3 for buildings built later than 1981, has created a need to evaluate the radon risk caused by the ground. Radon risk mapping is done both on a regional scale and a detailed scale. When mapping, the ground is classified into high, normal and low risk areas. The classification work is started by an interpretation of all available geological material from the investigated area. This is followed by field investigations including radon measurements in possible risk areas, and control of radium content by gamma spectrometry in the typical rock types and soil types of the area. Results from MRM Konsult's radon measurements show a very large increase of high radon houses within high risk areas, classified according to the above model, if compared to randomly distributed measurements.


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