期刊
GEOCHIMICA ET COSMOCHIMICA ACTA
卷 238, 期 -, 页码 394-410出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.gca.2018.07.018
关键词
Hydroxyl radical; Pyrite; Oxidation; Surface; Hydrogen peroxide
资金
- Applied Science and Technology Research and Development Project of Guangdong Province, China [2016B020240008]
- Natural Science Foundation of China (NSFC) [41772374, 41521001]
- Natural Science Foundation of Hubei Province, China [2018CFA028]
- high-performance computing platform of China University of Geosciences
Pyrite oxidation by hydrogen peroxide (H2O2) occurs in both natural and engineered systems. Hydroxyl radical (center dot OH) is a key reactive intermediate for pyrite and coexisting substances oxidation. In acidic H2O2/pyrite systems, H2O2 decomposition by aqueous Fe2+ is documented to predominate for center dot OH production, whereas here we show that H2O2 decomposition by sur- face Fe(II) sites contributes considerably to center dot OH production under certain conditions. Pyrite oxidation by H2O2 under anoxic conditions was performed under different conditions (2-12 g/L pyrite, 0.025-1 mM H2O2 and pH 2-4), and center dot OH and aqueous Fe2+/Fe3+ production as well as H(2)O(2 )consumption were measured during the oxidation. In order to evaluate the contribution of surface reaction to center dot OH production, 1 mM 2, 2'-bipyridine (BPY) was added to inhibit H2O2 decomposition by aqueous Fe2+. The rate constants of center dot OH production decreased by 44.4-65.6% with addition of 1 mM BPY, which suggests that both surface and aqueous reactions contributed to center dot OH production. Regarding the surface reaction, density functional theory (DFT) calculation reveals that H2O2 was adsorbed onto the Fe(II) sites on pyrite surface and transformed to surface adsorbed center dot OH which desorbed subsequently into the aqueous solution. On the basis of mechanistic understanding, a kinetic model was developed to assess the relative contributions of surface and aqueous reactions to center dot OH production. The relative contribution of surface reaction is dependent on the ratio of pyrite surface concentration to aqueous Fe2+ concentration, which decreases with the progress of pyrite oxidation due to the increase in aqueous Fe2+. When the ratio is higher than the threshold value of 1.6 x 10(3) m(2)/mM, surface reaction becomes predominant for 'OH production. Typical systems necessitating consideration of surface reaction involve pyritic rocks and shale leaching and pollutants treatment by H2O2/pyrite. The mechanisms unraveled in this study supplement the fundamental of center dot OH production from pyrite oxidation by both H2O2 and O-2 in natural and engineered systems. (C) 2018 Elsevier Ltd. All rights reserved.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据