Role of Carbonate in Thermodynamic Relationships Describing Pollutant Reduction Kinetics by Iron Oxide-Bound Fe2+

被引:14
|
作者
Chen, Gongde [1 ]
Hofstetter, Thomas B. [2 ,3 ]
Gorski, Christopher A. [1 ]
机构
[1] Penn State Univ, Dept Civil & Environm Engn, University Pk, PA 16802 USA
[2] Swiss Fed Inst Aquat Sci & Technol, Eawag, CH-8600 Dubendorf, Switzerland
[3] Swiss Fed Inst Technol, Swiss Fed Inst Technol, Inst Biogeochem & Pollutant Dynam IBP, CH-8092 Zurich, Switzerland
基金
美国国家科学基金会; 瑞士国家科学基金会;
关键词
NITROGEN ISOTOPE FRACTIONATION; NATURAL ORGANIC-MATTER; ABIOTIC REDUCTION; SURFACE CATALYSIS; REDOX PROPERTIES; STRUCTURAL FE; FERROUS IRON; METAL-IONS; FE(II); COMPLEXATION;
D O I
10.1021/acs.est.0c02959
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The reduction of environmental pollutants by Fe2+ bound to iron oxides is an important process that determines pollutant toxicities and mobilities. Recently, we showed that pollutant reduction rates depend on the thermodynamic driving force of the reaction in a linear free energy relationship that was a function of the solution pH value and the reduction potential, EH, of the interfacial Fe3+/Fe2+ redox couple. In this work, we studied how carbonate affected the free energy relationship by examining the effect that carbonate has on nitrobenzene reduction rates by Fe2+ bound to goethite (alpha-FeOOH). Carbonate slowed nitrobenzene reduction rates by inducing goethite particle aggregation, as evidenced by surface charge and particle size measurements. We observed no evidence for carbonate affecting Fe3+/Fe2+ reduction potentials or the mechanism of nitrobenzene reduction. The linear free energy relationship accurately described the data collected in the presence of carbonate when we accounted for the effect it had on the reactive surface area of goethite. The findings from this work provide a framework for determining why common groundwater constituents affect the E-H-dependence of reaction rates involving oxide-bound Fe2+ as a reductant.
引用
收藏
页码:10109 / 10117
页数:9
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