B33E-0780
Influence of urbanization on radon potential in Zhongshan City in the southern China

Wednesday, 16 December 2015
Poster Hall (Moscone South)
Nanping Wang, China University of Geosciences, School of Geophysics and Tecnology, Beijing, China
Abstract:
Radon and radon progeny are the most important contribution to dose from natural sources of radiation. Most studies have demonstrated an increased risk of lung cancer at high concentration of radon for the public. Radon potential map is an essential approach for radon risk assessment.

The radon potential map is based on the measured data of soil gas radon concentration and soil air permeability, combined with GIS technology, in Zhongshan City in the Southern China. The preliminary radon survey in ZC was conducted using a portable semiconductor radon monitor RAD-7 and soil air permeability instrument Rad-jok, covering a total area of 1800 km2. The sampling depth for soil gas radon measurement in the field was at the depth of 80 cm below the ground. 222Rn activity concentrations varyed between 0.74 and 158 kBq/m3, and 220Rn between 0.02 and 235 kBq/m3 in soil gas. The average value of 222Rn and 220Rn was 67.6 and 74.8 kBq/m3, respectively. The results show that: (1) the characteristics and distributions of 222Rn/220Rn concentration from soil gas in ZC are obviously related with local lithology (the Middle and the Late Jurassic and the Cretaceous biotitic-granite) and geological formation. High 222Rn/220Rn concentrations were observed in soil gas in the outcrops of weathered granite or filled back granite sands. (2) The distribution model of 220Rn is as same as that of 222Rn. The Wuguishan Mountain areas and in the south-east areas of ZC, covering with granite rocks, are high radon risk districts; the central zones in ZC are low radon potential areas, and part of the northern districts are medium radon potential areas. (3) Urbanization has increased local radon risk in some districts in the west and the north of ZC, where now covering several meters depth weathered granite products, but deposited the Quaternary sediments near surface before.

The research was supported by National Natural Science Foundation of China (No. 41474107, No.41274133 and 41074096).