A density functional theory study of Fe(II)/Fe(III) distribution in single layer green rust: a cluster approach

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Weichao Sun, Dominique J. Tobler, Martin P. Andersson
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引用次数: 2

Abstract

Green rust (GR) is a potentially important compound for the reduction of heavy metal and organic pollutants in subsurface environment because of its high Fe(II) content, but many details of the actual reaction mechanism are lacking. The reductive capacity distribution within GR is a key to understand how and where the redox reaction occurs and computational chemistry can provide more details about the electronic properties of green rust. We constructed three sizes of cluster models of single layer GR (i.e., without interlayer molecules or ions) and calculated the charge distribution of these structures using density functional theory. We found that the Fe(II) and Fe(III) are distributed unevenly in the single layer GR. Within a certain range of Fe(II)/Fe(III) ratios, the outer iron atoms behave more like Fe(III) and the inner iron atoms behave more like Fe(II). These findings indicate that the interior of GR is more reductive than the outer parts and will provide new information to understand the GR redox interactions.

Abstract Image

单层绿锈中Fe(II)/Fe(III)分布的密度泛函理论研究:集群方法
绿锈(GR)因其高铁(Fe(II))含量而成为潜在的还原地下环境中重金属和有机污染物的重要化合物,但其实际反应机理尚缺乏详细的研究。GR内的还原容量分布是了解氧化还原反应发生的方式和位置的关键,计算化学可以提供更多关于绿锈电子特性的细节。我们构建了三种大小的单层GR簇模型(即没有层间分子或离子),并利用密度泛函理论计算了这些结构的电荷分布。我们发现Fe(II)和Fe(III)在单层GR中分布不均匀,在一定的Fe(II)/Fe(III)比值范围内,外层铁原子的行为更像Fe(III),而内部铁原子的行为更像Fe(II)。这些发现表明GR的内部比外部更具有还原性,并将为理解GR的氧化还原相互作用提供新的信息。
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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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