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稀土尾矿砂放射性活度的测量与计算分析

苑超 周程 朱晓翔 杨师俨 戴耀东

苑超, 周程, 朱晓翔, 杨师俨, 戴耀东. 稀土尾矿砂放射性活度的测量与计算分析[J]. 原子核物理评论, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460
引用本文: 苑超, 周程, 朱晓翔, 杨师俨, 戴耀东. 稀土尾矿砂放射性活度的测量与计算分析[J]. 原子核物理评论, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460
YUAN Chao, ZHOU Cheng, ZHU Xiaoxiang, YANG Shiyan, DAI Yaodong. Measurement and Calculation of Rare Earth Mine Tailings Radioactivity[J]. Nuclear Physics Review, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460
Citation: YUAN Chao, ZHOU Cheng, ZHU Xiaoxiang, YANG Shiyan, DAI Yaodong. Measurement and Calculation of Rare Earth Mine Tailings Radioactivity[J]. Nuclear Physics Review, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460

稀土尾矿砂放射性活度的测量与计算分析

doi: 10.11804/NuclPhysRev.32.04.460
详细信息
    通讯作者: 戴耀东

Measurement and Calculation of Rare Earth Mine Tailings Radioactivity

  • 摘要: 准确测量并计算稀土尾矿砂的放射性活度浓度及其变化规律对制定相应的豁免标准和日后的处理处置具有重要的意义。根据选取的特征 射线,分析对比平衡与非平衡状态下铀系、钍系、锕系三个天然衰变系的总活度浓度,结合衰变链的一般动力学方程,计算总放射性活度与每个核素的放射性活度,并研究钍系各核素在平衡被不同程度破坏的情况下随时间的变化规律。结果显示,按照非平衡情况下计算得出的总α 和总β 放射性活度浓度比平衡情况下的更接近实际测量结果,此外,钍系核素在平衡被破坏后的放射性活度随时间变化情况与母体和228Ra 的初始放射性活度浓度有关,若228Ra 小于232Th,则总放射性活度在60 a再次平衡后达到最大值,为10 倍的母体活度;若228Ra 大于232Th,则总放射性活度在3.82 a 出现最大值,为4.57 倍母体活度与5.25 倍第一子体228Ra 的初始活度浓度之和。因此,可知稀土尾矿砂放射性活度已经遭到破坏,其总活度浓度应该采用非平衡情况下的几个特征核素的活度浓度共同计算得到,并且需计算分析其
    随时间变化出现的最大值,以此来确定是否超过相关法规标准。

    It is of great significance to measure and calculate rare earth tailing radioactivity for the development of appropriate standards and exemption disposal. The total activity concentration of the three natural decay series (uranium series, thorium series, actinium series) was analyzed under the equilibrium and disequilibrium state according to the selected characteristic  γ-rays. At the same time, we calculated the total activity concentration and the radioactivity for each radionuclide based on the general kinetic equations of decay chain and studied the trend of each radionuclide of thorium-series under different degrees of disequilibrium with time. The results demonstrated that the total radioactivity of and calculated in disequilibrium state was more closed to the actual measurement results compared to that in equilibrium state. In addition, the activity changes with time of thorium series in disequilibrium state are related to the initial activity concentration of the mother nuclide and 228Ra. If the activity concentration of 228Ra is less than that of 232Th, the total activity peak will be 10 times to maternal activity and appear after 60 a when the thorium series become balance again. If the activity concentration of 228Ra is greater than that of 232Th, the maximum total activity will appear in 3.82 a, and will be the sum of 4.57 times of the initial activity concentration of the mother nuclide and 5.25 times of the initial activity concentration of the first daughter 228Ra. Therefore, the rare earth tailings have been in disequilibrium state, and its total activity concentration should be determined based on the activity concentration of several  feature radionuclides. In addition, the maximum value of the activity concentration is profitable to judge whether the activity concentration is fit with relevant regulations and standards.
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出版历程
  • 收稿日期:  2015-01-02
  • 录用日期:  2015-12-20
  • 刊出日期:  2015-12-20

稀土尾矿砂放射性活度的测量与计算分析

doi: 10.11804/NuclPhysRev.32.04.460
    通讯作者: 戴耀东

摘要: 准确测量并计算稀土尾矿砂的放射性活度浓度及其变化规律对制定相应的豁免标准和日后的处理处置具有重要的意义。根据选取的特征 射线,分析对比平衡与非平衡状态下铀系、钍系、锕系三个天然衰变系的总活度浓度,结合衰变链的一般动力学方程,计算总放射性活度与每个核素的放射性活度,并研究钍系各核素在平衡被不同程度破坏的情况下随时间的变化规律。结果显示,按照非平衡情况下计算得出的总α 和总β 放射性活度浓度比平衡情况下的更接近实际测量结果,此外,钍系核素在平衡被破坏后的放射性活度随时间变化情况与母体和228Ra 的初始放射性活度浓度有关,若228Ra 小于232Th,则总放射性活度在60 a再次平衡后达到最大值,为10 倍的母体活度;若228Ra 大于232Th,则总放射性活度在3.82 a 出现最大值,为4.57 倍母体活度与5.25 倍第一子体228Ra 的初始活度浓度之和。因此,可知稀土尾矿砂放射性活度已经遭到破坏,其总活度浓度应该采用非平衡情况下的几个特征核素的活度浓度共同计算得到,并且需计算分析其
随时间变化出现的最大值,以此来确定是否超过相关法规标准。

It is of great significance to measure and calculate rare earth tailing radioactivity for the development of appropriate standards and exemption disposal. The total activity concentration of the three natural decay series (uranium series, thorium series, actinium series) was analyzed under the equilibrium and disequilibrium state according to the selected characteristic  γ-rays. At the same time, we calculated the total activity concentration and the radioactivity for each radionuclide based on the general kinetic equations of decay chain and studied the trend of each radionuclide of thorium-series under different degrees of disequilibrium with time. The results demonstrated that the total radioactivity of and calculated in disequilibrium state was more closed to the actual measurement results compared to that in equilibrium state. In addition, the activity changes with time of thorium series in disequilibrium state are related to the initial activity concentration of the mother nuclide and 228Ra. If the activity concentration of 228Ra is less than that of 232Th, the total activity peak will be 10 times to maternal activity and appear after 60 a when the thorium series become balance again. If the activity concentration of 228Ra is greater than that of 232Th, the maximum total activity will appear in 3.82 a, and will be the sum of 4.57 times of the initial activity concentration of the mother nuclide and 5.25 times of the initial activity concentration of the first daughter 228Ra. Therefore, the rare earth tailings have been in disequilibrium state, and its total activity concentration should be determined based on the activity concentration of several  feature radionuclides. In addition, the maximum value of the activity concentration is profitable to judge whether the activity concentration is fit with relevant regulations and standards.

English Abstract

苑超, 周程, 朱晓翔, 杨师俨, 戴耀东. 稀土尾矿砂放射性活度的测量与计算分析[J]. 原子核物理评论, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460
引用本文: 苑超, 周程, 朱晓翔, 杨师俨, 戴耀东. 稀土尾矿砂放射性活度的测量与计算分析[J]. 原子核物理评论, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460
YUAN Chao, ZHOU Cheng, ZHU Xiaoxiang, YANG Shiyan, DAI Yaodong. Measurement and Calculation of Rare Earth Mine Tailings Radioactivity[J]. Nuclear Physics Review, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460
Citation: YUAN Chao, ZHOU Cheng, ZHU Xiaoxiang, YANG Shiyan, DAI Yaodong. Measurement and Calculation of Rare Earth Mine Tailings Radioactivity[J]. Nuclear Physics Review, 2015, 32(4): 460-466. doi: 10.11804/NuclPhysRev.32.04.460

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