核化学与放射化学2024,Vol.46Issue(5) :499-505.DOI:10.7538/hhx.2024.46.05.0499

北山地下水中三元铀酰配合物的化学种态分析

Chemical Species Analysis of Ternary Uranyl Complexes in Groundwater of Beishan

吴思远 陈亚雯 郭宁 李杰彪 田强
核化学与放射化学2024,Vol.46Issue(5) :499-505.DOI:10.7538/hhx.2024.46.05.0499

北山地下水中三元铀酰配合物的化学种态分析

Chemical Species Analysis of Ternary Uranyl Complexes in Groundwater of Beishan

吴思远 1陈亚雯 2郭宁 2李杰彪 3田强1
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作者信息

  • 1. 西南科技大学环境友好能源材料国家重点实验室,材料与化学学院,四川绵阳 621010
  • 2. 北京分子科学国家研究中心,放射化学与辐射化学重点学科实验室,北京大学化学与分子工程学院,北京 100871
  • 3. 核工业北京地质研究院,北京 100029
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摘要

获知地下水环境中放射性核素的化学种态,对于理解其吸附、迁移和扩散行为至关重要.利用水文地球化学模拟软件PHREEQC,计算了 BS03(pH=9.43)和BS05(pH=7.51)两种北山深部地下水中铀(铀酰)的种态分布,重点分析了 pH、温度和初始铀浓度等因素的影响.研究结果表明,铀在弱酸性条件下,主要以UO2CO3(aq)和(UO2)2CO3(OH)3-存在;在中性至弱碱性条件下,主要以CaUO2(CO3)32-和Ca2UO2(CO3)3(aq)存在,且碳酸铀酰钙的含量远高于碳酸铀酰镁.随着温度的升高,Ca2UO2(CO3)3(aq)、CaUO2(CO3)32-和UO2(CO3)34-逐渐分解.当初始铀浓度为4×10-4~1×10-1mmol/L时(t=25 ℃),北山深部地下水中铀的优势种态为Ca2UO2(CO3)3(aq)(摩尔分数x>62%)和CaUO2(CO3)32-(x≈35%)三元配合物.研究结果对于分析关键放射性元素铀在高水平放射性废物处置库中的释放和迁移机制具有重要作用.

Abstract

Due to anthropogenic and long-term geological factors,radionuclide leakage may occur in deep geological repositories of radioactive waste when groundwater infiltrates a failed waste canister.The released radionuclides can migrate to near and far field regions through groundwater,posing a serious threat to the ecological environment and human health.As a consequence,knowledge of radionuclide speciation in groundwater is essential for understanding their transport behavior.Uranium is one of the key elements of significant concern for deep geological disposal of high-level radioactive waste.In this study,the uranium species in groundwater from boreholes BS03(pH=9.43)and BS05(pH=7.51)located at the Beishan area(Gansu province)were calculated by the hydrogeochemical software PHREEQC(version 3).The effects of pH,temperature,and initial uranium concentrations on ternary uranyl species are presented.The results indicate that UO2CO3(aq)and(UO2)2CO3(OH)3-are the dominant species in a mildly acidic condition,while CaUO2(CO3)32-and Ca2UO2(CO3)3(aq)are the major species in neutral and weakly alkaline conditions.In BS05 groundwater,the concentration of Ca2+(5.11 mmol/L)is about three times higher than that of Mg2+(1.58 mmol/L).However,the concentration of calcium uranyl carbonate is estimated to be about 250 times higher than that of magnesium uranyl carbonate(MgUO2(CO3)32-).With an increase of temperature,Ca2UO2(CO3)3(aq),CaUO2(CO3)32-and UO2(CO3)34-concentrations progressively diminish.At uranium concentrations between 4×10-4 and 1×10-1 mmol/L(25 ℃),the dominant uranium species,in order of decreasing concentration are:Ca2UO2(CO3)3(aq)(x>62%)>CaUO2(CO3)32-(x≈ 35%)>MgUO2(CO3)32-/UO2(CO3)34-(x≈ 1%),irrespective of the concentrations of Ca2+,Mg2+,and Na+.In the near-neutral and slightly alkaline conditions,the results suggest that the formation of neutral Ca2UO2(CO3)3(aq)and anionic CaUO2(CO3)32-in Beishan groundwater reduces the distribution coefficient between uranium and environmental geo-medium,thereby enhancing the mobility and migration potential of uranium.The research findings contribute to understanding the transport and release mechanisms of uranium,as well as interactions between uranium species and engineered and natural barriers.

关键词

碳酸铀酰钙/种态分布/PHREEQC/北山地下水

Key words

calcium-uranyl-carbonate/distribution of species/PHREEQC/Beishan groundwater

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出版年

2024
核化学与放射化学
中国核学会核化学与放射化学学会

核化学与放射化学

CSTPCDCSCD北大核心
影响因子:0.347
ISSN:0253-9950
参考文献量31
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