Study of long term radon transport by measuring the difference of the 210Pb and 226Ra activity in soil as a function of the depth.
Long term radon transport has been studied by measuring the activity difference of 210Pb and 226Ra in soil as a function of the depth. The results are from test pits of 1-2 m depth made at a dam of a tailings pond and at the plateau of a waste rock pile. Soil samples of about 1 kg were taken at a successive distances of 5 cm and analyzed by means of gamma-ray spectroscopy using low background germanium n-type detectors. It is shown that by this method nearly model independent information about the radon transport over a period of several decades can be inferred from the data.
Schulz
H
H
Radioökologie GmbH Dresden, Karpatenstr. 20, 01326 Dresden, Germany. schulz@iaf-dresden.de
Funke
L
L
Schellenberger
A
A
D004777:Environment; D055593:Geological Phenomena; D005844:Geology; D005858:Germany; D007856:Lead Radioisotopes / Q000032:analysis*; D008962:Models, Theoretical; D011883:Radium / Q000032:analysis*; D011886:Radon / Q000032:analysis*; D012990:Soil Pollutants, Radioactive / Q000032:analysis*
D007856:Lead Radioisotopes; D012990:Soil Pollutants, Radioactive; D011886:Radon; D011883:Radium