PRB去除模拟地下水中六价铬的反应特性

Reactivity Characteristics of Hexavalent Chromium Removed by PRB in Simulated Ground Water

  • 摘要: 采用粒径为0.15~0.42 mm的零价铁(Fe0)和粒径为0.15 mm的活性炭(AC)作为PRB反应介质,通过连续流动试验研究Fe0/AC-PRB修复模拟污染地下水时反应介质与六价铬〔Cr(Ⅵ)〕的反应特性,分析了AC对Cr(Ⅵ)的去除作用、Fe0对Cr(Ⅵ)的还原作用及其氧化还原产物、Fe0/AC对Cr(Ⅵ)的协同去除效果,研究了土壤中残留铬的形态。结果表明,在进水pH为6.9~7.1条件下,AC对Cr(Ⅵ)有一定的去除作用,主要通过吸附对Cr(Ⅵ)加以去除。Fe0对Cr(Ⅵ)有较高的去除率,进水Cr(Ⅵ)浓度为10 mg/L时,去除率达96%,氧化还原产物Fe3+和Cr3+与OH-形成沉淀附着在反应介质中,不会迁移到“下游”水体。Fe0/AC电池腐蚀反应可以提高Fe0的还原能力和还原效率,相对于Fe0单独作用时,铬铁比提高了1倍以上,出水pH从原水的7.0上升到8.0左右,铁浓度小于0.20 mg/L。经过去离子水冲洗,容易迁移且易于被生物利用的弱酸可提取态铬解吸到水相中,有机物与硫化物结合态和残渣态是含水层土壤中铬的主要存在形态,从生物可利用角度来说,铬的环境风险大大降低。

     

    Abstract: The zero-valent iron (Fe0) with particle size of 0.15-0.42 mm and the activated carbon (AC) with particle size of 0.15 mm were used as PRB reaction mediums. By continuous flow simulation experiments, the reactivity characteristics and removal effect of hexavalent chromium (Cr(Ⅵ)) contaminated ground water by Fe0/AC-PRB were investigated. The removal effect of Cr(Ⅵ) by AC, the reducing action of Cr(Ⅵ) by Fe0 and their redox products of chromium deoxidized, and collaborative removal effect of Fe0/AC were analyzed, and the speciation of chromium remained in aquifer was investigated. The results showed that Cr(Ⅵ) was removed to some extend mainly by adsorption under the conditions of influent pH 6.9-7.1. Meanwhile, the chromium could be deoxidized by Fe0 more effectively, with the efficiency up to 96% while continuously inputting simulated groundwater containing 10 mg/L hexavalent chromium. During the process, the redox products, Fe3+ and Cr3+, were precipitated on the reaction medium; therefore they did not transfer into downstream water. Micro-electrolysis improved the reduction capacity and efficiency of Fe0, and compared with the effect of sole Fe0, the ratio of chromium to iron increased by more than 1 time, the pH increased from 7.0 of influent to 8.0 of effluent, and the total iron concentration of effluent was below 0.20 mg/L. Chromium was easily transported and extracted by bioavailable weak acid when the aquifer was flushed with deionized water. Chromium was distributed mainly in organic/sulphide fractions and residue fraction, which indicated that a low ecological risk of chromium remained in aquifer to environment.

     

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