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Coupled Iron Corrosion and Chromate Reduction: Mechanisms for Subsurface Remediation

机译:铁腐蚀与铬酸盐还原耦合:地下修复的机制

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The reduction of chromium from the Cr(Ⅵ) to the Cr-(Ⅲ) state by the presence of elemental, or zero-oxidation-state, iron metal was studied to evaluate the feasibility of such a process for subsurface chromate remediation. Reactions were studied in systems of natural aquifer materials with varying geochemistry. Different forms of iron metal had significantly different abilities to reduce chromate, ranging from extremely rapid to essentially no effect. Impure, partially oxidized iron was most effective, with iron quantity being the most important rate factor, followed by aquifer material type and solid:solution ratio. Evidence for chromium-iron hydroxide solid solution (Cr_x,Fe_(1-X))(OH)_3(ss) formation was obtained by electron probe microanalysis. A cyclic, multiple reaction electrochemical corrosion mechanism, enhanced by the development of an electrical double-layer analogue, is proposed to explain the differing iron reactivities and aquifer material effects.
机译:研究了通过元素金属或零氧化态铁金属的存在将铬从Cr(Ⅵ)还原为Cr-(Ⅲ)的方法,以评估这种方法用于地下铬酸盐修复的可行性。在具有不同地球化学性质的天然含水层系统中研究了反应。不同形式的铁金属具有显着不同的还原铬酸盐的能力,范围从极快到基本上没有。不纯的,部分氧化的铁最有效,铁的数量是最重要的速率因子,其次是含水层的材料类型和固溶比。通过电子探针显微分析获得了铬铁氢氧化物固溶体(Cr_x,Fe_(1-X))(OH)_3(ss)的证据。提出了通过双层电子类似物的开发增强的循环,多反应电化学腐蚀机理,以解释不同的铁反应性和含水层材料的影响。

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