Asgharizadeh F, Ghannadi M, Samani A B, Meftahi M, Shalibayk M, Sahafipour S A, Gooya E S
Nuclear Science and Technology Research Institute, AEOI, PO Box 11365-3486, Tehran, Iran.
Radiat Prot Dosimetry. 2013 Sep;156(3):376-82. doi: 10.1093/rpd/nct067.
The study was carried out to determine radioactivity concentrations in surface soil samples of the city of Tehran and associated potential radiological hazards. The natural radionuclide ((226)Ra, (232)Th and (40)K) contents were determined for 50 locations throughout the geological surface formations in a representative area in the city of Tehran, Iran, using high-resolution gamma-spectrometric analysis. The range of activity concentrations of (226)Ra, (232)Th and (40)K in the soil from the studied areas varies from 30.5±0.6 to 45.4±0.9, 27.3±0.5 to 57.1±1.1 and 328.0±4.6 to 768.5±13.4 Bq kg(-1) with overall mean values of 38.8±0.7, 43.4±0.8 and 555.1±8.9 Bq kg(-1), respectively. The mean radium equivalent activity, external hazard index, internal hazard index to quantify the internal exposure to radon and its daughter products, as well as the gamma activity concentration index for each sample are 143.6±4.6 Bq kg(-1), 0.39, 0.49 and 0.53, respectively. The average estimated radium equivalent is comparable with reported values for many countries in the world. Therefore, these areas may not pose radiological risks to the inhabitants due to harmful effects of the ionising radiation from the natural radioactivity in soil. The calculated average external and internal hazard indexes were found to be less than unity, as a recommended safe level. Estimates of the measured radionuclide content have been made for calculating the absorbed dose rate in the outdoor air at 1 m above the ground level. The absorbed dose rates resulting from those concentrations ranged from 48.1 to 88.7 nGy h(-1). Assuming a 20 % occupancy factor proposed by UNSCEAR, 2000, the corresponding effective dose rates in outdoor air equivalent to the population were calculated to be between 0.06 and 0.11 mSv y(-1). The measurement results and calculated values obtained from this study indicate that the dwelling areas in Tehran city, Iran, have background radioactivity levels within natural limits.
开展本研究以确定德黑兰市表层土壤样品中的放射性浓度及相关潜在放射性危害。利用高分辨率伽马能谱分析,测定了伊朗德黑兰市一个代表性区域内50个地质表层形成位置的天然放射性核素(镭 - 226、钍 - 232和钾 - 40)含量。研究区域土壤中镭 - 226、钍 - 232和钾 - 40的活度浓度范围分别为30.5±0.6至45.4±0.9、27.3±0.5至57.1±1.1以及328.0±4.6至768.5±13.4 Bq kg⁻¹,总体平均值分别为38.8±0.7、43.4±0.8和555.1±8.9 Bq kg⁻¹。每个样品的镭当量活度均值、外照射危害指数、用于量化氡及其子体内部照射的内照射危害指数以及伽马活度浓度指数分别为143.6±4.6 Bq kg⁻¹、0.39、0.49和0.53。估算的镭当量平均值与世界上许多国家报告的值相当。因此,由于土壤中天然放射性产生的电离辐射的有害影响,这些区域可能不会对居民构成放射性风险。计算得出的平均外照射和内照射危害指数均小于1,这是推荐的安全水平。已对测量的放射性核素含量进行估算,以计算地面上方1米处室外空气中的吸收剂量率。这些浓度产生的吸收剂量率范围为48.1至88.7 nGy h⁻¹。假设采用联合国原子辐射效应科学委员会2000年提出的20%占用因子,计算得出相当于人群的室外空气中相应有效剂量率在0.06至0.11 mSv y⁻¹之间。本研究获得的测量结果和计算值表明,伊朗德黑兰市的居住区放射性背景水平处于天然限值范围内。