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氨基酸对水滑石固定硒酸盐释放的环境影响:实验与密度泛函理论研究的综合解释。

Environmental impact of amino acids on the release of selenate immobilized in hydrotalcite: Integrated interpretation of experimental and density-functional theory study.

机构信息

Department of Earth Resources Engineering, Kyushu University, Fukuoka, 819-0395, Japan.

Department of Applied Chemistry, Kyushu University, Fukuoka, 819-0395, Japan.

出版信息

Chemosphere. 2021 Jul;274:129927. doi: 10.1016/j.chemosphere.2021.129927. Epub 2021 Feb 15.

Abstract

The environmental impact of amino acids on the release of SeO immobilized into hydrotalcite (MgAl-LDH) which belongs to the layered double hydroxides (LDHs) family was investigated by experimental study and the observed layer structure of hydrotalcite was verified through density-functional theory (DFT) calculations. Glycine, l-cysteine, and l-aspartic acid, which have smaller molecular sizes, can release SeO largely due to intercalation, unstabilization of MgAl-LDH and simple dissolution, while l-tryptophan and l-phenylalanine caused limited SeO release due to their larger sizes and aromaticity. XRD patterns for the solid residues after intercalation of amino acids revealed that the layer distance of MgAl-LDH was partially expanded. The main peaks and shoulder features corresponding to d diffraction were well explained by DFT simulations using glycine as a model: the layer spacing of the main peak is responsible for the remaining SeO and singly stacked glycine molecule and the layer spacing of the shoulder peak was well explained by doubly stacked glycine molecules. Hydrogen bonds between amino acids and hydroxyl ions in the metallic layers of MgAl-LDH were responsible for the stable configuration of the intercalated MgAl-LDH. This study indicates potential limitations to the stability of low-level radioactive wastes of Se in repositories which are affected by smaller molecules of amino acids released through degradation of organic matters in the pedosphere.

摘要

通过实验研究考察了氨基酸对硒氧固定在属于层状双氢氧化物(LDHs)家族的水滑石(MgAl-LDH)中释放的环境影响,并通过密度泛函理论(DFT)计算验证了所观察到的水滑石的层状结构。由于插层、MgAl-LDH 的不稳定性和简单溶解,甘氨酸、l-半胱氨酸和 l-天冬氨酸等分子尺寸较小的氨基酸可以大量释放 SeO,而 l-色氨酸和 l-苯丙氨酸由于其较大的尺寸和芳香性,导致 SeO 的释放有限。氨基酸插层后固体残留物的 XRD 图谱表明,MgAl-LDH 的层间距部分扩大。使用甘氨酸作为模型进行 DFT 模拟很好地解释了对应于 d 衍射的主峰和肩峰特征:主峰的层间距负责剩余的 SeO 和单堆叠甘氨酸分子,而肩峰的层间距很好地解释了双堆叠甘氨酸分子。氨基酸和 MgAl-LDH 金属层中羟基离子之间的氢键负责插层 MgAl-LDH 的稳定构型。这项研究表明,在土壤中有机物降解释放的较小分子氨基酸的影响下,储存库中硒的低放废物的稳定性可能存在潜在限制。

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