Central Department of Physics, Tribhuvan University, Kathmandu, 44600, Bagmati, Nepal.
Department of Physics, Amrit Campus, Tribhuvan University, Kathmandu, 44600, Bagmati, Nepal.
Environ Monit Assess. 2024 Jan 23;196(2):190. doi: 10.1007/s10661-023-12284-5.
Soil samples from vegetable farmland in densely populated wards of Nepal were analyzed for natural radionuclide levels, employing a NaI(Tl) 3" [Formula: see text] 3" gamma detector. The study aimed to evaluate the causes of radiation risk, attributing it to soil contamination resulting from the rapid urbanization and concretization that followed the earthquake in 2015. The activity concentration of radium-226, thorium-232, and potassium-40 and the ranges observed are 2.080±0.084-33.675±1.356 Bq kg[Formula: see text], 17.222±0.198-119.949±1.379 Bq kg[Formula: see text], and 11.203 ± 0.325-748.828±21.716 Bq kg[Formula: see text], respectively. The average values obtained for hazard indices are as follows: radium equivalent activity (82.779 Bq kg[Formula: see text]), absorbed dose rate (36.394 nGy h[Formula: see text]), annual effective dose equivalent (0.045 mSv yearr[Formula: see text]), gamma index (0.291), external hazard index (0.224), internal hazard index (0.253), excess lifetime cancer risk (0.159), annual gonadal dose equivalent (243.278 mSv year[Formula: see text]), alpha index (0.054), and activity utilization index (0.716). However, in most places, thorium-232 concentration is greater than those of the world average and recommended values. In specific locations such as Ward 4 in Baluwatar, the soil was found to have concentrations of Ra[Formula: see text] and K[Formula: see text] exceeding recommended limits. Despite this localized concern, the overall analysis of hazard indices across the studied areas revealed that most values were within permissible limits. This suggests that, on a broader scale, radiation exposure may not be a significant concern in the investigated regions. Nonetheless, the study recommends regular monitoring in additional locations to ensure a comprehensive and ongoing assessment of radiation levels.
从尼泊尔人口密集区的菜地土壤样本中,采用 NaI(Tl) 3" [Formula: see text] 3" 伽马探测器分析天然放射性核素水平。该研究旨在评估辐射风险的原因,将其归因于 2015 年地震后快速城市化和混凝土化导致的土壤污染。镭-226、钍-232 和钾-40 的活度浓度及其观察到的范围分别为 2.080±0.084-33.675±1.356 Bq kg[Formula: see text]、17.222±0.198-119.949±1.379 Bq kg[Formula: see text] 和 11.203 ± 0.325-748.828±21.716 Bq kg[Formula: see text]。获得的危害指数平均值如下:镭当量活度(82.779 Bq kg[Formula: see text])、吸收剂量率(36.394 nGy h[Formula: see text])、年有效剂量当量(0.045 mSv yearr[Formula: see text])、伽马指数(0.291)、外部危害指数(0.224)、内部危害指数(0.253)、过量寿命癌症风险(0.159)、年性腺剂量当量(243.278 mSv year[Formula: see text])、α指数(0.054)和活度利用指数(0.716)。然而,在大多数地方,钍-232 的浓度大于世界平均值和推荐值。在特定地点,如 Baluwatar 的第 4 区,土壤中的 Ra[Formula: see text] 和 K[Formula: see text] 浓度超过了推荐限值。尽管存在这种局部担忧,但对研究区域的危害指数进行的总体分析表明,大多数值都在允许范围内。这表明,在更广泛的范围内,辐射暴露可能不是调查区域的一个重要问题。尽管如此,该研究仍建议在其他地点进行定期监测,以确保对辐射水平进行全面和持续的评估。