Woda Clemens, Jacob P, Ulanovsky A, Fiedler I, Mokrov Y, Rovny S
Institute of Radiation Protection, Helmholtz Zentrum München, German Research Center for Environmental Health, 85764, Neuherberg, Germany.
Radiat Environ Biophys. 2009 Nov;48(4):405-17. doi: 10.1007/s00411-009-0236-x. Epub 2009 Aug 13.
Recently discovered historical documents indicate that large releases of noble gases (mainly (41)Ar and radioactive isotopes of Kr and Xe) from the Mayak Production Association (MPA) over the period from 1948 to 1956 may have caused considerable external exposures of both, inhabitants of Ozyorsk and former inhabitants of villages at the upper Techa River. To quantify this exposure, seven brick samples from three buildings in Ozyorsk, located 8-10 km north-northwest from the radioactive gas release points, were taken. The absorbed dose in brick was measured in a depth interval of 3-13 mm below the exposed surface of the bricks by means of the thermoluminescence (TL) and the optically stimulated luminescence (OSL) method. Generally, luminescence properties using TL were more favorable for precise dose determination than using OSL, but within their uncertainties the results from both methods agree well with each other. The absorbed dose due to natural radiation was assessed and subtracted under the assumption of the bricks to be completely dry. The weighted average of the anthropogenic dose for all samples measured by TL and OSL is 10 +/- 9 and 1 +/- 9 mGy, respectively. An upper limit for a possible anthropogenic dose in brick that would not be detected due to the measurement uncertainties is estimated at 24 mGy. This corresponds to an effective dose of about 21 mSv. A similar range of values is obtained in recently published dispersion calculations that were based on reconstructed MPA releases. It is concluded that the release of radioactive noble gases from the radiochemical and reactor plants at Mayak PA did not lead to a significant external exposure of the population of Ozyorsk. In addition, the study demonstrates the detection limit for anthropogenic doses in ca. 60-year-old bricks to be about 24 mGy, if luminescence methods are used.
最近发现的历史文献表明,1948年至1956年期间,玛雅克生产协会(MPA)大量释放惰性气体(主要是(^{41})Ar以及Kr和Xe的放射性同位素),可能导致奥焦尔斯克居民以及捷恰河上游村庄的原居民受到相当程度的外部照射。为了量化这种照射,从位于放射性气体释放点西北偏北8 - 10公里处的奥焦尔斯克三座建筑物中采集了七个砖块样本。通过热释光(TL)和光激发发光(OSL)方法,在砖块暴露表面以下3 - 13毫米的深度区间测量砖块中的吸收剂量。一般来说,使用TL的发光特性比使用OSL更有利于精确测定剂量,但在测量不确定度范围内,两种方法的结果相互吻合良好。在假设砖块完全干燥的情况下,评估并扣除了天然辐射产生的吸收剂量。通过TL和OSL测量的所有样本的人为剂量加权平均值分别为10±9和1±9毫戈瑞。由于测量不确定度而未被检测到的砖块中可能的人为剂量上限估计为24毫戈瑞。这相当于约21毫希沃特的有效剂量。在最近发表的基于重建的MPA释放量的扩散计算中也得到了类似的值范围。得出的结论是,玛雅克PA的放射化学和反应堆工厂释放的放射性惰性气体并未导致奥焦尔斯克居民受到显著的外部照射。此外,该研究表明,如果使用发光方法,对于约60年历史的砖块中人为剂量的检测限约为24毫戈瑞。