Tokonami Shinji, Sun Quanfu, Akiba Suminori, Zhuo Weihai, Furukawa Masahide, Ishikawa Tetsuo, Hou Changsong, Zhang Shouzhi, Narazaki Yukinori, Ohji Baku, Yonehara Hidenori, Yamada Yuji
Radon Research Group, Research Center for Radiation Safety, National Institute of Radiological Sciences, 4-9-1 Anagawa, Inage, Chiba 263-8555, Japan.
Radiat Res. 2004 Oct;162(4):390-6. doi: 10.1667/rr3237.
Measurements of natural radiation were carried out in cave dwellings distributed in the Chinese loess plateau. Those dwellings are located in Shanxi and Shaanxi provinces. Radon and thoron gas concentrations were measured using a passive integrating radon-thoron discriminative detector. Concentrations of thoron decay products were estimated from measurements of their deposition rates. A detector was placed at the center of each dwelling for 6 months and replaced with a fresh one for another 6 months. Measurements were conducted in 202 dwellings from August 2001 through August 2002. A short-term measurement was conducted during the observation period. In addition, gamma-ray dose rates were measured both indoors and outdoors with an electronic pocket dosimeter. Radioactivities in soil were determined by gamma-ray spectrometry with a pure germanium detector. Among 193 dwellings, indoor radon concentrations ranged from 19 to 195 Bq m(-3) with a geometric mean (GM) of 57 Bq m(-3), indoor thoron concentrations ranged from 10 to 865 Bq m(-3) with a GM of 153 Bq m(-3), and indoor equilibrium equivalent thoron concentrations ranged from 0.3 to 4.9 Bq m(-3) with a GM of 1.6 Bq m(-3). Arithmetic means of the gamma-ray dose rates were estimated to be 140 nGy h(-1) indoors and 110 nGy h(-1) outdoors. The present study revealed that the presence of thoron is not negligible for accurate radon measurements and thus that special attention should be paid to thoron and its decay products for dose assessment in such an environment. More systematic studies are necessary for a better understanding of thoron and its decay products.
在中国黄土高原分布的窑洞内进行了天然辐射测量。这些窑洞位于山西和陕西省。使用被动式积分氡 - 钍鉴别探测器测量氡和钍气浓度。钍衰变产物的浓度通过测量其沉积率来估算。在每个窑洞的中心放置一个探测器6个月,然后更换一个新的探测器再测量6个月。在2001年8月至2002年8月期间,对202个窑洞进行了测量。在观测期内进行了短期测量。此外,使用电子袖珍剂量计在室内和室外测量了γ射线剂量率。用高纯锗探测器通过γ射线能谱法测定土壤中的放射性。在193个窑洞当中,室内氡浓度范围为19至195 Bq m(-3),几何平均值(GM)为57 Bq m(-3);室内钍浓度范围为10至865 Bq m(-3),GM为153 Bq m(-3);室内钍平衡当量浓度范围为0.3至4.9 Bq m(-3),GM为1.6 Bq m(-3)。γ射线剂量率的算术平均值估计在室内为140 nGy h(-1),在室外为110 nGy h(-1)。本研究表明,对于准确的氡测量,钍的存在不可忽略,因此在这样的环境中进行剂量评估时,应特别关注钍及其衰变产物。需要进行更系统的研究以更好地了解钍及其衰变产物。