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Field-scale bioremediation of arsenic-contaminated groundwater using sulfate-reducing bacteria and biogenic pyrite

机译:还原硫酸盐细菌和生物黄铁矿对砷污染地下水的现场规模生物修复

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This research demonstrates that biogenic pyrite formed by stimulation of indigenous sulfate-reducing bacteria (SRB) in a natural aquifer can remove dissolved arsenic from contaminated groundwater under strongly reducing conditions. SRB metabolism led to the precipitation of biogenic pyrite nanoparticles capable of sorbing and co-precipitating arsenic. The field site is an industrial site where shallow groundwater in an unconfined sandy aquifer is contaminated by arsenic. Therefore, biodegradable organic carbon, ferrous iron, sulfate, and fertilizer were injected into groundwater and SRB metabolism began about 1 week later. Microscopic, X-ray diffraction, X-ray fluorescence, and electron microprobe analyses confirm the bio-mineralization of pyrite and over time, pyrite nanoparticles grew to form well-formed crystals (1-10 mu m in diameter) or spherical aggregates that contain 0.05-0.4 wt. % arsenic, indicative of their capacity to sequester arsenic. Consequently, dissolved arsenic decreased from its initial concentration of 0.3-0.5 mg/L to below the regulatory clean-up standard for the site of 0.05 mg/L in three downgradient wells in a matter of weeks after injection. The main sequestration stage, with total arsenic removal rates greater than 90%, lasted for at least 6 months until the arrival and mixing of untreated groundwater from upgradient. Treated groundwater with most active bacterial sulfate reduction became enriched in heavy S-34 (range from 2.02 to 4.00 parts per thousand) compared to unaffected well water (0.40-0.61 parts per thousand). One to three orders of magnitude increases in SRB cells were observed in treated wells for at least 2 months after injection. For a full-scale remediation, the injection of solution should start at positions hydrologically upgradient from the major plume and proceed downgradient. If needed, aquifers may be repeatedly amended with biodegradable organic carbon to reestablish the reducing conditions that favor arsenic sequestration.
机译:这项研究表明,通过刺激天然含水层中的原生硫酸盐还原细菌(SRB)形成的生物黄铁矿可以在强烈还原的条件下从受污染的地下水中去除溶解的砷。 SRB代谢导致能够吸附和共沉淀砷的生物黄铁矿纳米颗粒沉淀。现场是工业现场,无约束的含沙含水层中的浅层地下水被砷污染。因此,将可生物降解的有机碳,亚铁,硫酸盐和化肥注入地下水,约1周后开始SRB代谢。显微镜,X射线衍射,X射线荧光和电子探针分析证实了黄铁矿的生物矿化作用,随着时间的推移,黄铁矿纳米粒子生长形成了良好形成的晶体(直径为1-10微米)或球形聚集体,其中含有0.05-0.4重量砷百分比,表明其螯合砷的能力。因此,在注入后的数周内,三个下降井中的溶解砷从其初始浓度0.3-0.5 mg / L下降到低于法规清理标准的0.05 mg / L浓度。主要的固存阶段(总砷去除率大于90%)持续至少6个月,直到未升级的地下水到达并混合为止。与未受影响的井水(千分之0.40-0.61)相比,处理后的具有最有效的细菌硫酸盐还原作用的地下水变得富含重S-34(千分之2.0至4.00份)。注射后至少2个月,在处理过的孔中观察到SRB细胞增加了1-3个数量级。为了进行全面修复,溶液的注入应从主要羽状流在水文学上逐渐升级的位置开始,然后逐步降低。如果需要,可以用可生物降解的有机碳反复修正含水层,以建立有利于砷固存的还原条件。

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