A41A-0052
Seasonal Variation of Unattached fraction and Equilibrium factor of 222Rn and 220Rn using DRPS/DTPS and Pin –hole cup dosimeters.

Thursday, 17 December 2015
Poster Hall (Moscone South)
Pargin Bangotra, Rohit Mehra and Rajan Jakhu, National Institute of Technology jalandhar, Physics, Jalandhar, India
Abstract:
222Rn (Radon), 220Rn (Thoron) and their progenies are naturally occurring radionuclides in environment and responsible for the radiological dose to population. The 222Rn, 220Rn concentration and their separate attached and unattached progeny concentration (season-wise) in units of EEC have been measured in the dwellings of Muktsar and Mansa districts of Punjab (India), using Pin- hole cup dosimeters and deposition based progeny sensors (DTPS/DRPS). The indoor 222Rn concentration was maximum in the rainy season (60 Bqm-3) while 220Rn concentration was maximum in winter season (57 Bqm-3). However EEC of 222Rn and 220Rn has distinct seasonal demeanour than their parent nuclides. The unattached EEC for both 222Rn and 220Rn (EERCU and EETCU) were higher in summer and rainy season as compared to winter season. The equilibrium factor ( for 222Rn and for 220Rn) and unattached fraction ( for 222Rn and for 220Rn) has been calculated separately. The (0.44 ± 0.04) in the studied area was similar to 0.4 that proposed by UNSCEAR and for (0.05 ± 0.01) it was greater than specified value 0.02 by UNSCEAR. The was higher in summer season as compared to rainy and winter season. Due to very smaller value of , a proper relation has not been observed seasonally. The unattached fraction in environment may increase the risk of radiological exposure and absorbed at faster rate into blood then the attached 222Rn and 220Rn progeny. The overall arithmetic mean (rainy, winter and summer seasons) of and were 0.09 ± 0.02 and 0.10 ± 0.03 respectively. The and were lower in winter season as compared to rainy and summer seasons due to higher value of attached EEC present in winter season. A positive and significant correlation (0.56) has been observed between the and aerosol concentration (Z (cm-3)).