Key Laboratory of Agricultural Engineering in Structure and Environment of Ministry of Agricultural, College of Water Conservancy & Civil Engineering, China Agricultural University, 100083 Beijing, PR China.
Water Res. 2012 Apr 15;46(6):1923-32. doi: 10.1016/j.watres.2012.01.011. Epub 2012 Jan 20.
Long-term investigations were carried out in two pilot-scale horizontal subsurface flow constructed wetlands (planted and unplanted) with an iron-rich soil matrix for treating sulphate-rich groundwater which was contaminated with low concentrations of chlorinated hydrocarbons. The temporal and spatial dynamics of pore-water sulphide, Fe(II) and phosphate concentrations in the wetland beds were characterized and the seasonal effects on sulphide production and nitrification inhibition were evaluated. The results demonstrated that the pore-water sulphide concentrations gradually increased from less than 0.2 mg/L in 2005 to annual average concentrations of 15 mg/L in 2010, while the pore-water Fe(II) concentrations decreased from 35.4 mg/L to 0.3 mg/L. From 2005 to 2010, the phosphate removal efficiency declined from 91% to 10% under a relatively constant inflow concentration of 5 mg/L. The pronounced effect of plants was accompanied by a higher sulphate reduction and ammonium oxidation in the planted bed, as compared to the unplanted control. A high tolerance of plants towards sulphide toxicity was observed, which might be due to the detoxification of sulphide by oxygen released by the roots. However, during the period of 2009-2010, the nitrification was negatively impacted by the sulphide production as the reduction in the removal of ammonium from 75% to 42% (with inflow concentration of 55 mg/L) correlated with the increasing mean annual sulphide concentrations. The effect of the detoxification of sulphide and the immobilization of phosphate by the application of the iron-rich soil matrix in the initial years was proven; however, the life-span of this effect should not only be taken into consideration in further design but also in scientific studies.
长期调查在两个带有富铁土壤基质的中试规模水平潜流人工湿地(种植和未种植)中进行,用于处理受低浓度氯化碳污染的富含硫酸盐的地下水。湿地床中孔隙水硫化物、Fe(II)和磷酸盐浓度的时空动态特征以及季节性对硫化物产生和硝化抑制的影响进行了评估。结果表明,孔隙水硫化物浓度从 2005 年的低于 0.2mg/L 逐渐增加到 2010 年的年平均浓度 15mg/L,而孔隙水 Fe(II)浓度从 35.4mg/L 降低到 0.3mg/L。2005 年至 2010 年期间,在 5mg/L 相对恒定的入流浓度下,磷酸盐去除效率从 91%下降到 10%。与未种植对照相比,种植床中硫酸盐还原和铵氧化的效果更为显著。观察到植物对硫化物毒性具有较高的耐受性,这可能是由于根系释放的氧气对硫化物进行了解毒。然而,在 2009-2010 年期间,由于去除铵的比例从 75%下降到 42%(入流浓度为 55mg/L),与孔隙水中年平均硫化物浓度的增加相关,硝化受到硫化物产生的负面影响。证明了富铁土壤基质在初期应用中对硫化物的解毒和磷酸盐的固定的效果;然而,不仅在进一步的设计中,而且在科学研究中,都应该考虑到这种效果的寿命。