中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Molecular simulation on Cs, Rb retention in Na/K-montmorillonite interlayer coupling clay swelling/collapse

文献类型:期刊论文

作者Zhou, Mengzi2; Lu, Xiancai2; Chen, Meng1; Li, Qin2; Wang, Kai2; Liu, Xiandong2
刊名APPLIED GEOCHEMISTRY
出版日期2025
卷号178页码:15
关键词Cs Rb Retention Cation selectivity Montmorillonite Molecular simulation
ISSN号0883-2927
DOI10.1016/j.apgeochem.2024.106249
英文摘要A key issue about radioactive waste disposal and nuclear accident contamination control is the retention of radionuclides in clay minerals. The cation (Cs+, Rb+, Na+, K+) selectivity in montmorillonite (Mt) interlayers have not been quantitatively studied. This work employs classical molecular dynamics (CMD) to systematically investigate the interlayer structure, swelling properties, diffusion dynamics, and cation exchange processes. The selectivity of alkali ions within the interlayer space coupled with clay swelling/collapse under different water activity (a(w)) and cation activity, has been quantified. Both Cs-, Rb-Mt demonstrate a monolayer hydrate configuration as the most stable state. The mobility of intercalated species, as indicated by self-diffusion coefficients, exhibits a stepwise trend with increasing water content. The cationic selectivity within the interlayer follows the order Cs+ > Rb+ > K+ > Na (+) at a(w) = 1.0. The logarithm values of the selectivity coefficients for Cs/Rb relative to Na/K are as follows: logK(c)(Cs/K) = 0.73, logK(c)(Cs/Na) = 1.62, logK(c)(Rb/K) = 0.62, and logK(c)(Rb/Na) = 1.57 at a(w) = 1.0. A model correlating selectivity coefficients with water activity has been proposed. It is noted that Cs+ and Rb+ ions tend to accumulate within the interlayer as water activity decreases, and interlayer Rb+ competes with Cs+ for exchange positions at low water activity. These results can be used to quantify cationic partitioning during the remediation of radiocesium contamination in soil and weathering processes of sediments.
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:001378881600001
源URL[http://ir.gig.ac.cn/handle/344008/81899]  
专题中国科学院矿物学与成矿学重点实验室
通讯作者Lu, Xiancai
作者单位1.Chinese Acad Sci, Inst Earth Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny,Guangdong Prov Key L, Guangzhou 510640, Peoples R China
2.Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, Sch Earth Sci & Engn, State Key Lab Ore Deposits Res, Nanjing 210023, Jiangsu, Peoples R China
推荐引用方式
GB/T 7714
Zhou, Mengzi,Lu, Xiancai,Chen, Meng,et al. Molecular simulation on Cs, Rb retention in Na/K-montmorillonite interlayer coupling clay swelling/collapse[J]. APPLIED GEOCHEMISTRY,2025,178:15.
APA Zhou, Mengzi,Lu, Xiancai,Chen, Meng,Li, Qin,Wang, Kai,&Liu, Xiandong.(2025).Molecular simulation on Cs, Rb retention in Na/K-montmorillonite interlayer coupling clay swelling/collapse.APPLIED GEOCHEMISTRY,178,15.
MLA Zhou, Mengzi,et al."Molecular simulation on Cs, Rb retention in Na/K-montmorillonite interlayer coupling clay swelling/collapse".APPLIED GEOCHEMISTRY 178(2025):15.

入库方式: OAI收割

来源:广州地球化学研究所

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