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硒(IV)与膨润土微生物群落相互作用对铜腐蚀及硒形态的双重影响:对储存库安全评估的启示

Dual effect of Se(IV) and bentonite microbial community interactions on the corrosion of copper and Se speciation: Implication on repository safety assessment.

作者信息

Martinez-Moreno Marcos F, Povedano-Priego Cristina, Morales-Hidalgo Mar, Mumford Adam D, Lazuen-Lopez Guillermo, Aranda Elisabet, Vilchez-Vargas Ramiro, Solari Pier L, Ju-Nam Yon, Jroundi Fadwa, Ojeda Jesus J, Merroun Mohamed L

机构信息

Faculty of Sciences, Department of Microbiology, University of Granada, Granada, Spain.

Faculty of Sciences, Department of Microbiology, University of Granada, Granada, Spain.

出版信息

Sci Total Environ. 2025 Feb 15;965:178613. doi: 10.1016/j.scitotenv.2025.178613. Epub 2025 Jan 30.

Abstract

The Deep Geological Repository (DGR) design, the internationally safest option for the long-term disposal of high-level radioactive waste (HLW), features metal canisters encased in compacted bentonite clay and embedded deep within a host rock. Despite presenting a hostile environment for microorganisms, DGRs scenarios with favorable microbial-activity conditions must be considered for the safety assessment of this disposal. This study investigated the impact of Se(IV), as a natural analogue of Se present in the HLW, in anoxic microcosms of bentonite slurry spiked with a bacterial consortium and amended with lactate, acetate, and sulfate as electron donors/acceptor. The addition of the bacterial consortium promoted the rate of Se(IV) reduction to Se(0), while the tyndallization (heat-shock) of bentonite slowed this process. Se(IV) reduced the relative abundance of most genera of sulfate-reducing bacteria (SRB), while stimulating the abundance of Se-tolerant bacteria, which played an important role in Se(IV) reduction. Moreover, it was observed that lactate was the preferred electron donor, linking to the production and subsequent consumption of acetate. X-ray absorption spectroscopy (XAS) and high-resolution transmission electron microscopy (HRTEM) revealed the reduction of Se(IV) forming amorphous Se(0) nanospheres. In addition, HRTEM showed that the biogenic Se(0) undergo a biotransformation to more stable crystalline forms, contributing to the immobilization of Se in the case of HLW release. Additionally, the sulfide generated by the activity of SRB reacted with Cu producing corrosion products (CuS) on the surface of the copper material.

摘要

深部地质处置库(DGR)设计是国际上高放废物(HLW)长期处置最安全的选择,其特点是金属罐包裹在压实的膨润土中,并深埋于主岩中。尽管DGR对微生物来说是一个恶劣的环境,但在对这种处置方式进行安全评估时,必须考虑具有有利微生物活性条件的DGR情景。本研究调查了作为HLW中硒天然类似物的硒(IV),在添加了细菌群落并用乳酸、乙酸和硫酸盐作为电子供体/受体进行修正的膨润土泥浆缺氧微观世界中的影响。添加细菌群落促进了硒(IV)还原为硒(0)的速率,而膨润土的间歇灭菌(热休克)减缓了这一过程。硒(IV)降低了大多数硫酸盐还原菌(SRB)属的相对丰度,同时刺激了耐硒细菌的丰度,这些细菌在硒(IV)还原中起重要作用。此外,观察到乳酸是首选的电子供体,这与乙酸的产生和随后的消耗有关。X射线吸收光谱(XAS)和高分辨率透射电子显微镜(HRTEM)揭示了硒(IV)还原形成无定形硒(0)纳米球。此外,HRTEM表明生物源硒(0)会发生生物转化为更稳定的晶体形式,在HLW释放的情况下有助于硒的固定。此外,SRB活动产生的硫化物与铜反应,在铜材料表面产生腐蚀产物(CuS)。

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