Structures and acidity constants of arsenite and thioarsenite species in hydrothermal solutions

被引：16

作者：

Liu, Xiandong ^{[1
]}

He, Mengjia ^{[1
]}

Lu, Xiancai ^{[1
]}

Wang, Rucheng ^{[1
]}

机构：

[1] Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposit Res, Nanjing 210093, Jiangsu, Peoples R China

来源：

CHEMICAL GEOLOGY | 2015年 / 411卷

基金：

美国国家科学基金会;

关键词：

First principles molecular dynamics; Arsenite; Thioarsenite; Speciation; Acidity constant; Hydration structure; INITIO MOLECULAR-DYNAMICS; MOLAL THERMODYNAMIC PROPERTIES; SURFACE-ACIDITY; METAL COMPLEXATION; AQUEOUS-SOLUTION; DEGREES-C; SULFIDE; FLUIDS; SPECIATION; MINERALS;

D O I：

10.1016/j.chemgeo.2015.07.015

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

We report a first principles molecular dynamics (FPMD) study of structures and acidity constants of arsenite and thioarsenite species in liquid water from ambient temperature to 573 K. The analyses show that at all temperatures, the OH ligands of arsenite species form H-bonds with solvating water molecules as both donors and acceptors, whereas there are only very weak H-bonds between the SH ligands of thioarsenite species and water. For both arsenites and thioarsenites, the dangling O/S sites form strong H-bonds with hydrogen atoms of water molecules, but the As atoms have almost no interaction with water molecules. The FPMD based vertical energy gap method was applied to calculate the acidity constants. With the evaluated acidity, the species distributions with respect to pH have been derived. The pK(a1)s of H3AsO3 and H3AsS3 demonstrate a decreasing trend with temperature. For arsenites, H3AsO3 and H2AsO3- can coexist, whereas HAsO32- almost does not exist, due to the notably high pK(a2)s of H3AsO3. For thioarsenites, H2AsS3- and HAsS32- are always the dominant species in the near neutral pH range from ambient temperature to 573 K. (C) 2015 Elsevier B.V. All rights reserved.

引用

页码：192 / 199

页数：8