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不同花岗岩组成材料中锶分布系数的差异及其意义。

Differences and implications of strontium distribution coefficient on various granite compositional materials.

机构信息

College of Construction Engineering, Jilin University, Changchun, 130026, China.

School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao, 266520, China.

出版信息

Environ Sci Pollut Res Int. 2024 Jul;31(35):47899-47910. doi: 10.1007/s11356-024-34351-1. Epub 2024 Jul 16.

DOI:10.1007/s11356-024-34351-1
PMID:39012533
Abstract

The distribution coefficient (K) of radionuclides is a crucial parameter in assessing the safety of high-level radioactive waste (HLW) geological repository. It is determined in the laboratory through batch and column experiments. However, differences in obtained K values from distinct experiments have not been thoroughly assessed and compared. This study evaluated strontium (Sr) sorption on different granite materials using static batch and dynamic experiments (column and core-flooding experiments). The results from batch sorption experiments showed higher Sr sorption on granite under acidic and strongly alkaline conditions, low solid-liquid ratios, and low ionic strength. In column experiments, a two-site sorption model was used to simulate Sr transport in crushed granite and mixed pure minerals. The sorption of Sr on crushed granite exhibited a higher affinity than that of mixed pure minerals. The dual-porosity transport model was employed to investigate Sr transport behavior in fractured granite in the core-flooding experiment. K obtained from batch sorption experiments are four to twenty times higher than those from column experiments, and two to three orders of magnitude higher than that from a core-flooding experiment. The results of this study provide valuable insights into safety assessment for the HLW geological repository.

摘要

放射性核素的分配系数(K)是评估高放废物(HLW)地质处置库安全性的关键参数。它可以通过批量和柱实验在实验室中确定。然而,不同实验中获得的 K 值之间的差异尚未得到彻底评估和比较。本研究使用静态批量和动态实验(柱和岩心驱替实验)评估了不同花岗岩材料对锶(Sr)的吸附。批量吸附实验的结果表明,在酸性和强碱性条件下、低固液比和低离子强度下,Sr 在花岗岩上的吸附更高。在柱实验中,使用双位点吸附模型模拟了 Sr 在破碎花岗岩和混合纯矿物中的运移。Sr 在破碎花岗岩上的吸附比混合纯矿物的吸附具有更高的亲和力。双孔隙度输运模型用于研究岩心驱替实验中裂隙花岗岩中 Sr 的输运行为。批量吸附实验中获得的 K 值比柱实验高 4 到 20 倍,比岩心驱替实验高 2 到 3 个数量级。本研究的结果为 HLW 地质处置库的安全评估提供了有价值的见解。

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