Zhou Xian, Zhang Zheng-Fu, Bao Chong-Jun, Chen Man-Jiao, Pan Gechuanqi, Wan Rundong, Wang Jin-Song, Liu Yang, Yang Hui
Faculty of Materials Science and Engineering, Kunming University of Science and Technology, Kunming650093, China.
Kunming Metallurgical Research Institute Company Limited, Kunming650031, China.
Langmuir. 2023 Jan 11. doi: 10.1021/acs.langmuir.2c02545.
Lollingite (FeAs) is considered an arsenic-bearing mineral that is oxidized faster than arsenopyrite. The geometric configuration, chemical valence bond, and microscopic reaction of the oxidation on the surface of lollingite were systematically studied, which are of great significance for understanding the mechanism of oxidative dissolution. X-ray photoelectron spectroscopy (XPS) measurements and density functional theory (DFT) calculations were carried out to characterize the (101) surface oxidation process of lollingite under the O/O + HO conditions. XPS results confirmed that the participation of water molecules can promote the formation of abundant OH structures on the surface of lollingite, while the relative concentration of O, As(III), and Fe(III) increased. Moreover, the DFT results demonstrated that the (101) As-terminal plane of FeAs was the most stable surface with the lowest surface energy. HO molecules were physically adsorbed onto the Fe atoms of the lollingite surface, while oxygen molecules can readily be adsorbed on the Fe-As site by chemical adsorption processes. The oxidation process of the lollingite surface with water includes the following mechanisms: adsorption, dissociation, formation of the hydrogen bond, and desorption. The dissociation of the HO molecule into OH and H led to the hydroxylation of both Fe and As atoms and the formation of hydrogen bonding. The participation of HO molecules can also reduce the reaction energy barrier and accelerate the oxidation reaction of the lollingite surface, especially as far as the water dissociation and formation of hydrogen bonds are concerned. According to PDOS data, there is considerable hybridization between the d orbitals of bonded Fe atoms and the p orbitals of O atoms, as well as between the p orbitals of bonded As atoms and the p orbitals of O atoms. Due to a strong propensity for orbital hybridization and bonding between the s orbitals of the H atoms in HO molecules and the p orbitals of the O atoms on the (101) surface, water molecules have the ability to speed up the oxidation on the surface.
黄铁矿(FeAs)被认为是一种含砷矿物,其氧化速度比毒砂快。系统研究了黄铁矿表面氧化的几何构型、化学键和微观反应,这对于理解氧化溶解机理具有重要意义。通过X射线光电子能谱(XPS)测量和密度泛函理论(DFT)计算,对O/O + HO条件下黄铁矿(101)表面的氧化过程进行了表征。XPS结果证实,水分子的参与可以促进黄铁矿表面形成丰富的OH结构,同时O、As(III)和Fe(III)的相对浓度增加。此外,DFT结果表明,FeAs的(101)As端平面是表面能最低、最稳定的表面。HO分子物理吸附在黄铁矿表面的Fe原子上,而氧分子可以通过化学吸附过程容易地吸附在Fe-As位点上。黄铁矿表面与水的氧化过程包括以下机制:吸附、解离、氢键形成和解吸。HO分子解离成OH和H导致Fe和As原子的羟基化以及氢键的形成。HO分子的参与还可以降低反应能垒,加速黄铁矿表面的氧化反应,特别是在水解离和氢键形成方面。根据PDOS数据,键合的Fe原子的d轨道与O原子的p轨道之间以及键合的As原子的p轨道与O原子的p轨道之间存在相当大的杂化。由于HO分子中H原子的s轨道与(101)表面O原子的p轨道之间有很强的轨道杂化和键合倾向,水分子有能力加速表面的氧化。