Title of article :
In situ gamma spectroscopy to characterize building materials as radon and thoron sources
Author/Authors :
Cristina Nuccetelli، نويسنده , , Chiara Bolzan، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2001
Pages :
6
From page :
355
To page :
360
Abstract :
In situ gamma spectroscopy is widely utilized to determine the outdoor gamma dose rate from the soil and to calculate the natural and artificial radionuclide concentration and their contribution to the dose rate. The application of in situ gamma spectroscopy in indoor environments can not supply quantitative information about activity concentration of radionuclides in building materials, but this technique can provide interesting information about building materials as radon source. In fact, a method based on analyses of gamma spectra data has been developed by the authors to provide, in field, quantitative estimation of disequilibrium in 226Ra and 228Ac sub-chains due to 222Rn and 220Rn exhalation. The method has been applied to data of gamma spectroscopy measurements carried out with HPGe detector Ž26%. in seven dwellings and one office in Rome. The first results of the data analysis show that, as regards especially the 226Ra sub-chain disequilibrium, different building materials Žtuff, concrete, etc.. can show very different characteristics. If, in addition to the spectrometric data, other indoor environment parameters Žindoor dose rates, room dimensions, wall thickness, etc.. ŽBochicchio et al., Radiat Prot Dosim 1994;56Ž1 4.:137 140; Bochicchio et al., Environ Int 1996a;22:S633 S639. are utilized in a room model, an evaluation of 226Ra, 228Ac and 40K activity concentration and an indication of the exhalation features, by means of estimation of exhaled 222Rn activity concentration, can be achieved.
Keywords :
building materials , Indoor gamma dose rate , Room model , 222Rn exhalation
Journal title :
Science of the Total Environment
Serial Year :
2001
Journal title :
Science of the Total Environment
Record number :
982635
Link To Document :
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