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使用可渗透反应屏障处理矿山排水:柱实验

Treatment of mine drainage using permeable reactive barrers: column experiments.

作者信息

Waybrant K R, Ptacek C J, Blowes D W

机构信息

Department of Earth Sciences, University of Waterloo, Ontario, Canada.

出版信息

Environ Sci Technol. 2002 Mar 15;36(6):1349-56. doi: 10.1021/es010751g.

Abstract

Permeable reactive barriers designed to enhance bacterial sulfate reduction and metal sulfide precipitation have the potential to prevent acid mine drainage and the associated release of dissolved metals. Two column experiments were conducted using simulated mine-drainage water to assess the performance of organic carbon-based reactive mixtures under controlled groundwater flow conditions. The simulated mine drainage is typical of mine-drainage waterthat has undergone acid neutralization within aquifers. This water is near neutral in pH and contains elevated concentrations of Fe(II) and SO4. Minimum rates of SO4 removal averaged between 500 and 800 mmol d(-1) m(-3) over a 14-month period. Iron concentrations decreased from between 300 and 1200 mg/L in the influent to between <0.01 and 220 mg/L in the columns. Concentrations of Zn decreased from 0.6-1.2 mg/L in the input to between 0.01 and 0.15 mg/L in the effluent, and Ni concentrations decreased from between 0.8 and 12.8 mg/L to <0.01 mg/L. The pH increased slightly from typical input values of 5.5-6.0 to effluent values of 6.5-7.0. Alkalinity, generally <50 mg/L (as CaCO3) in the influent, increased to between 300 and 1,300 mg/L (as CaCO3) in the effluent from the columns. As a result of decreased Fe(II) concentrations and increased alkalinity, the acid-generating potential of the simulated mine-drainage water was removed, and a net acid-consuming potential was observed in the effluent water.

摘要

旨在增强细菌硫酸盐还原作用和金属硫化物沉淀的渗透性反应屏障,有潜力预防酸性矿山排水及相关溶解金属的释放。进行了两个柱实验,使用模拟矿山排水来评估在受控地下水流条件下基于有机碳的反应混合物的性能。模拟矿山排水是典型的在含水层内经过酸中和的矿山排水。这种水的pH接近中性,且含有较高浓度的Fe(II)和SO4。在14个月的时间里,SO4去除的最低速率平均在500至800 mmol d(-1) m(-3)之间。铁浓度从进水的300至1200 mg/L降至柱内的<0.01至220 mg/L。锌浓度从输入的0.6 - 1.2 mg/L降至流出物的0.01至0.15 mg/L,镍浓度从0.8至12.8 mg/L降至<0.01 mg/L。pH从典型的输入值5.5 - 6.0略有升高至流出物值6.5 - 7.0。碱度在进水时通常<50 mg/L(以CaCO3计),在柱的流出物中增至300至1300 mg/L(以CaCO3计)。由于Fe(II)浓度降低和碱度增加,模拟矿山排水的产酸潜力被消除,且在流出水中观察到净耗酸潜力。

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