某地下核设施场址地下水化学特征及其对水循环的指示意义

李杰彪; 梁修雨; 周志超; 赵敬波; 潘跃龙; 郭永海

doi:10.3799/dqkx.2022.425

Volume 49 Issue 3

Mar. 2024

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Article Navigation > Earth Science > 2024 > 49(3): 965-977

Li Jiebiao, Liang Xiuyu, Zhou Zhichao, Zhao Jingbo, Pan Yuelong, Guo Yonghai, 2024. Hydrochemical Characteristics and Its Significance to Groundwater Flow System at an Underground Nuclear Facility Site. Earth Science, 49(3): 965-977. doi: 10.3799/dqkx.2022.425

Citation:

Li Jiebiao, Liang Xiuyu, Zhou Zhichao, Zhao Jingbo, Pan Yuelong, Guo Yonghai, 2024. Hydrochemical Characteristics and Its Significance to Groundwater Flow System at an Underground Nuclear Facility Site. Earth Science, 49(3): 965-977. doi: 10.3799/dqkx.2022.425

Citation:

Li Jiebiao, Liang Xiuyu, Zhou Zhichao, Zhao Jingbo, Pan Yuelong, Guo Yonghai, 2024. Hydrochemical Characteristics and Its Significance to Groundwater Flow System at an Underground Nuclear Facility Site. Earth Science, 49(3): 965-977. doi: 10.3799/dqkx.2022.425

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Hydrochemical Characteristics and Its Significance to Groundwater Flow System at an Underground Nuclear Facility Site

doi: 10.3799/dqkx.2022.425

1.
School of Environment, Harbin Institute of Technology, Harbin 150090, China
2.
School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
3.
CAEA Innovation Center for Geological Disposal of High-Level Radioactive Waste, Beijing Research Institute of Uranium Geology, Beijing 100029, China
4.
China Nuclear Power Engineering Co., Ltd., Shenzhen 518000, China

Received Date: 2022-07-08
Available Online: 2024-04-12
Publish Date: 2024-03-25

Abstract

Abstract

Hydrochemical characteristics are one of the most critical evaluation factors for the site selection and long-term performance safety evaluation of nuclear facilities. Mathematical statistics, ion proportion method, isotope analysis method, and hydrogeochemical simulation were used in this paper to investigate hydrochemical characteristics of an underground nuclear facility site along the coast. Its hydrochemical characteristics, possible controls, groundwater recharge source, and apparent age were analyzed. Furthermore, the conceptual model of groundwater flow and hydrochemical evolution in the area was preliminarily constructed. The results suggest that the total dissolved solids (TDS) of the groundwater is low, and the pH value in most samples is weakly acidic. The hydrochemical types of groundwater sampling from boreholes and tunnels are mainly HCO₃-Na·Ca and HCO₃-Ca·Na. The weathering of silicate rocks specifically controls hydrochemical components. Moreover, the weathering dissolution of albite and anorthite is the primary water-rock interaction of groundwater along unconfined aquifer main runoff paths. The groundwater source is the infiltration recharge of local atmospheric precipitation, and the ¹⁴C apparent age in the depth range of nuclear facilities is about 2.08-3.60 ka. It is concluded that the hydrochemistry and groundwater circulation conditions at the site are beneficial to ensure the safety of underground nuclear facilities.
- hydrochemistry,
- ion source,
- hydrogeochemical modelling,
- isotope,
- nuclear facility site,
- groundwater

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References(50)

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Hydrochemical Characteristics and Its Significance to Groundwater Flow System at an Underground Nuclear Facility Site

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