Adsorption of water, sulfates and chloride on arsenopyrite surface

被引:26
|
作者
Silva, Juliana C. M. [1 ,2 ]
dos Santos, Egon C. [1 ]
de Oliveira, Aline [1 ]
Heine, Thomas [2 ,3 ]
De Abreu, Heitor A. [1 ]
Duarte, Helio A. [1 ]
机构
[1] Univ Fed Minas Gerais, Dept Quim, Grp Pesquisa Quim Inorgan Teor, ICEx, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil
[2] Jacobs Univ Bremen, Phys & Earth Sci, Campus Ring 1, D-28759 Bremen, Germany
[3] Univ Leipzig, Wilhelm Ostwald Inst Phys & Theoret Chem, Linnestr 2, D-04103 Leipzig, Germany
关键词
Arsenopyrite; Adsorption; Density functional theory; Plane waves; Sulfide minerals; Sulfates; OXIDATIVE DISSOLUTION; PYRITE; CHALCOPYRITE; MECHANISM; FEASS; REACTIVITY; CLEAVAGE; H2O;
D O I
10.1016/j.apsusc.2017.10.161
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Arsenopyrite is one of the sulfide minerals responsible for acid rock drainage (ARD) and is one of the most hazardous in regions affected by mining activities. This phenomenon involves complex reaction mechanism. Although it is intensely investigated, there is a lack of consensus concerning the reaction mechanisms and more information is still necessary. In this work, the adsorption of water, hydrochloric acid, and sulfuric acid on arsenopyrite (001) surface was investigated by means of Density Functional calculations and the results compared to other sulfides aiming to understand the mineral/ water interface. The interaction of the chemical species with the (001) FeAsS surface is the first step to understand the intricate oxidation mechanism of arsenopyrite. Molecular water adsorption on (001) FeAsS is more favored than the adsorption of sulfate favoring the dissolution of sulfates and enhancing its oxidation. The estimated adsorption energies of water, sulfates and chloride on other sulfide minerals are compared with the estimated values for arsenopyrite and the chemical reactivity differences discussed in detail. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:389 / 399
页数:11
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