估算尼日利亚三角洲州 Ethiope East 地区土壤向木薯的转移因子

E. F. Ejoh, A. Essiett, I. Essien, M. C. Bede, E. U. Benjamin, J. Atat
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引用次数: 0

摘要

木薯是三角洲州非常重要的主食作物。这项研究的目的是评估尼日利亚三角洲州 Ethiope 地方政府地区土壤中放射性核素的活度浓度水平,并确定其向木薯的转移因子。使用伽马能谱仪分析了从研究地区采集的土壤和木薯样本中 40K、238U 和 232Th 的放射性活度浓度。使用了一个铅屏蔽 3 x 3 英寸同轴型碘化钠铊[NaI(TI)]掺杂探测器晶体(型号 802 系列,堪培拉公司),通过前置放大器与堪培拉系列多通道分析仪(MCA)(型号 N0.1104)相连接。土壤样本的放射性浓度结果表明,40K 的平均放射性浓度最高((38.66 ± 3.69)BqKg-1),E2 的平均放射性浓度最高((62.47 ± 5.67)BqKg-1)。238U 和 232Th 的平均放射性浓度分别为 3.65 ± 0.90 BqKg-1 和 0.46 ± 0.05 BqKg-1。238U 和 232Th 的峰值分别为 5.07 ± 1.17 BqKg-1 和 0.98 ± 0.11 BqKg-1。木薯中的 40K 介于 75.06 至 200.08 BqKg-1 之间,其中 C5 的平均放射性浓度最高,为 99.62 ± 8.32 BqKg-1,最高值为 200.08 ± 14.90 BqKg-1。238U 和 232Th 的平均放射性浓度分别为 3.89 ± 0.93 BqKg-1 和 0.81 ± 0.09 BqKg-1。根据木薯样本的计算结果,238U 和 232Th 的最大值分别为 11.10 ± 2.48 BqKg-1 和 1.70 ± 0.18 BqKg-1。研究结果表明,研究地区土壤和木薯中 40K、238U 和 232Th 的放射性浓度分别低于 420、30 和 35 BqKg-1 的世界平均值,因此食用不会对人体造成危害。40K、238U 和 232Th 从土壤到木薯的平均转移因子分别为 3.12 ± 0.44、0.95 ± 0.31 和 2.96 ± 0.91。40K、238U 和 232Th 的数值范围分别为 1.41 至 5.82、BDL 至 2.98 和 0.21 至 9.35。40K 在 E8, C8 的峰值为 5.82,238U 在 E9, C9 的峰值为 2.98,232Th 在 E9, C9 的峰值为 9.35。TR值高的原因是土壤中含有丰富的有机物。天然放射性核素在土壤-岩浆岩中的快速循环表明存在内部循环,有助于天然放射性核素的积累。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of transfer factor from soil to cassava in Ethiope East, Delta State, Nigeria
Cassava is a very important staple food crop in Delta state. The aim of this research is to assess the activity concentration level and determine the transfer factor of radionuclide from soil to cassava in Ethiope Local Government Area of Delta state, Nigeria. The activity concentration of 40K, 238U and 232Th in soil and cassava samples collected from the study area were analysed using gamma spectrometry. A lead-shielded 3 x 3 inch coaxial type Sodium Iodide Thallium [NaI(TI)] doped detector crystal (Model No. 802 series, Canberra Inc.) coupled to a Canberra series multichannel Analyzer (MCA) (Model N0.1104) through a preamplifier was used. The results of the activity concentration in soil samples indicate that, 40K has the highest mean activity concentration ((38.66 ± 3.69) BqKg−1) with the highest value ((62.47 ± 5.67) BqKg−1) recorded at E2. The mean activity concentrations of 238U and 232Th are 3.65 ± 0.90 BqKg−1 and 0.46 ± 0.05 BqKg−1respectively. The peak values of 238U and 232Th are 5.07 ± 1.17 BqKg−1 and 0.98 ± 0.11 BqKg−1. From cassava, 40K varies from 75.06 to 200.08 BqKg−1 with the highest mean activity concentration of 99.62 ± 8.32 BqKg−1 and 200.08 ± 14.90 BqKg−1 as the highest value noted at C5. The mean activity concentrations of 238U and 232Th are 3.89 ± 0.93 BqKg−1 and 0.81 ± 0.09 BqKg−1 respectively. The maximum values of 238U and 232Th determined from the computation from cassava samples are 11.10 ± 2.48 BqKg−1 and 1.70 ± 0.18 BqKg−1. The results of this study show that the activity concentration of 40K, 238U and 232Th in the study area are lower than world average values of 420, 30 and 35 BqKg-1 in soil and cassava respectively, and it is therefore not harmful if consumed. The mean transfer factor of 40K, 238U and 232Th from soil to cassava are 3.12 ± 0.44, 0.95 ± 0.31 and 2.96 ± 0.91 respectively. The range of values of 40K, 238U and 232Th varied as 1.41 to 5.82, BDL to 2.98 and 0.21 to 9.35 correspondingly. Peak values of the TF were noted as 5.82 for 40K at E8, C8, 2.98 for 238U at at E9, C9 and 9.35 for 232Th at E9, C9. The high value of TR is accredited to the richness of the organic matter in the soil. The quick recycling of natural radionuclides through the soil-cassava suggests the presence of an internal cycling that help the build-up of the natural radionuclides.
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