State Key Lab of Biogeology and Environmental Geology, China University of Geosciences , 388 Lumo Road, Wuhan, 430074, P. R. China.
Environ Sci Technol. 2014 May 6;48(9):5145-53. doi: 10.1021/es500409m. Epub 2014 Apr 17.
Mobilization of Arsenic in groundwater is primarily induced by reductive dissolution of As-rich Fe(III) oxyhydroxides under anoxic conditions. Creating a well-controlled artificial environment that favors oxidative precipitation of Fe(II) and subsequent oxidation and uptake of aqueous As can serve as a remediation strategy. We reported a proof of concept study of a novel iron-based dual anode system for As(III) oxidation and removal in synthetic groundwater. An iron anode was used to produce Fe(II) under iron-deficient conditions, and another inert anode was used to generate O2 for oxidative precipitation of Fe(II). For 30 min's treatment, 6.67 μM (500 μg/L) of As(III) was completely oxidized and removed from the solution during the oxidative precipitation process when a total current of 60 mA was equally partitioned between the two anodes. The current on the inert anode determined the rate of O2 generation and was linearly related to the rates of Fe(II) oxidation and of As oxidation and removal, suggesting that the process could be manipulated electrochemically. The composition of Fe precipitates transformed from carbonate green rust to amorphous iron oxyhydroxide as the inert anode current increased. A conceptual model was proposed for the in situ application of the electrochemically induced oxidative precipitation process for As(III) remediation.
砷在地下水中的迁移主要是由缺氧条件下富砷 Fe(III)氢氧化物的还原溶解引起的。创造一个有利于 Fe(II)氧化沉淀以及随后的 As 水相氧化和吸收的良好控制的人工环境可以作为一种修复策略。我们报告了一种新型铁基双阳极系统用于模拟地下水中 As(III)氧化和去除的概念验证研究。铁阳极在缺铁条件下产生 Fe(II),而另一个惰性阳极用于产生 O2 以促进 Fe(II)的氧化沉淀。在 30 分钟的处理过程中,当 60 mA 的总电流在两个阳极之间平均分配时,溶液中的 6.67 μM(500 μg/L)的 As(III)在氧化沉淀过程中完全被氧化和去除。惰性阳极上的电流决定了 O2 的生成速率,并且与 Fe(II)氧化和 As 氧化和去除的速率呈线性关系,这表明该过程可以通过电化学进行控制。随着惰性阳极电流的增加,Fe 沉淀物的组成从碳酸绿锈转变为无定形铁氢氧化物。提出了一个用于原位应用电化学诱导氧化沉淀过程修复 As(III)的概念模型。