研究面依赖矿的氧化机制:对环境和硫的演变的影响
Chenrui Liu1, Yun Liu1, Shuai Zeng1
1Department of Environmental Science and Engineering, College of Environment and Resources, Xiangtan University, Xiangtan 411105, China. liuyunscut@163.com.
Environmental science. Processes & impacts
|October 16, 2023
概括
(FeS2) 的氧化率取决于暴露的晶体面. 皮里特矿是一种矿.
科学领域:
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
- 环境科学 环境科学
背景情况:
- 化氧化对环境和铁 (Fe) 和硫 (S) 元素的地球化学循环产生重大影响.
- 矿氧化的速度主要由其表面暴露的特定晶体面决定.
研究的目的:
- 为了研究自然存在的 (FeS2) (100) 和 (210) 水晶面的氧化行为和机制.
- 为了阐明石对氧的面体依赖反应性.
主要方法:
- 密度功能理论 (DFT) 计算建立吸附模型,计算表面能量,并确定FeS2100) 和FeS2210) 面上的氧吸附点和能量.
- 电化学技术包括电化学阻抗光谱 (EIS),表极化和循环电压测量 (CV) 来评估氧化速率.
- 化学氧化实验和X射线光电子光谱 (XPS) 分析,以量化氧化产品和识别中间硫物种.
主要成果:
- 与FeS2(100) 面相比,FeS2(210) 面表现出更高的对氧的反应性,这是由于更多的不和铁 (Fe) 原子.
- 电化学数据证实FeS2210) 的氧化率比FeS2100更快.
- 化学氧化和XPS分析显示,FeS2(210) 产生更多的总Fe,硫酸盐 (SO42-) 和质子 (H+),以及各种中间硫种.
结论:
- FeS2210) 面比FeS2100) 面更容易受到氧化的影响.
- 这项研究提供了基本的洞察力,以面依赖的氧化机制的pyrite.
- 这些发现有助于理解自然系统中铁和硫元素的地化学演变.
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