College of Resources and Environment & Chongqing Key Laboratory of Soil Multi-scale Interfacial Process, Southwest University, Chongqing 400715, China.
College of Resources and Environment & Chongqing Key Laboratory of Soil Multi-scale Interfacial Process, Southwest University, Chongqing 400715, China.
Environ Pollut. 2019 Nov;254(Pt B):113110. doi: 10.1016/j.envpol.2019.113110. Epub 2019 Aug 27.
Abiotic reduction represents an attractive technology to control U(VI) contamination. In this work, an abiotic route of U(VI) reduction with humic acid at mineral surfaces is proposed and reaction mechanisms are addressed by periodic density functional theory calculations. Different influencing factors such as ligand effect, content of CO ligands and substituent effect are inspected. The coordination chemistry of uranyl(VI) surface complexes relies strongly on substrates and ligands, and the calculated results are in good agreements with experimental observations available. For the OH ligand, two competitive mechanisms co-exist that respectively produce the U(IV) and U(V) species, and the former is significantly preferred because of lower energy barriers. Instead, the NO ligand leads to the formation of U(V) while for the Cl ligand, the U(VI) surface complex remains very stable and is not likely to be reduced because of very high energy barriers. The U(V) and U(IV) complexes are the predominant products for low and high CO contents, respectively. Accordingly, the abiotic reduction processes with humic acid are efficient to manage U(VI) contamination and become preferred under basic conditions or at higher CO contents. The U(VI) reduction is further promoted by introduction of electron-donating rather than electron-withdrawing substituents to humic acid. Electronic structure analyses and vibrational frequency assignments are calculated for the various uranium surface complexes of the reduction processes, serving as a guide for future experimental and engineered studies. The molecular-level understanding given in this work offers an abiotic route for efficient reduction of U(VI) and remediation of U(VI)-contaminated sites at ambient conditions.
在本工作中,提出了在矿物表面通过腐殖酸进行非生物 U(VI)还原的途径,并通过周期性密度泛函理论计算研究了反应机制。考察了配体效应、CO 配体含量和取代基效应等不同影响因素。铀酰(VI)表面配合物的配位化学强烈依赖于基质和配体,计算结果与现有实验观察结果吻合良好。对于 OH 配体,存在两种竞争性机制,分别生成 U(IV)和 U(V)物种,由于能垒较低,前者更占优势。而对于 NO 配体,则生成 U(V),对于 Cl 配体,由于能垒非常高,铀酰(VI)表面配合物仍然非常稳定,不易被还原。U(V)和 U(IV)配合物分别是低 CO 含量和高 CO 含量下的主要产物。因此,腐殖酸的非生物还原过程对于管理 U(VI)污染是有效的,并在碱性条件下或 CO 含量较高时成为首选。引入供电子取代基而不是吸电子取代基会进一步促进 U(VI)的还原。计算了还原过程中各种铀表面配合物的电子结构分析和振动频率分配,为未来的实验和工程研究提供了指导。本工作提供的分子水平理解为在环境条件下有效还原 U(VI)和修复 U(VI)污染场地提供了一种非生物途径。