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Engineered and subsequent intrinsic in situ bioremediation of a diesel fuel contaminated aquifer

机译:工程和随后的原位生物修复受柴油污染的含水层

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摘要

A diesel fuel contaminated aquifer in Menziken, Switzerland was treated for 4.5 years by injecting aerated groundwater, supplemented with KNO and NHHPO to stimulate indigenous populations of petroleum hydrocarbon (PHC) degrading microorganisms. After dissolved PHC concentrations had stabilized at a low level, engineered in situ bioremediation was terminated. The main objective of this study was to evaluate the efficacy of intrinsic in situ bioremediation as a follow-up measure to remove PHC remaining in the aquifer after terminating engineered in situ bioremediation. In the first 7 months of intrinsic in situ bioremediation, redox conditions in the source area became more reducing as indicated by lower concentrations of SO‾ and higher concentrations of Fe(II) and CH. In the core of the source area, strongly reducing conditions prevailed during the remaining study period (3 years) and dissolved PHC concentrations were higher than during engineered in situ bioremediation. This suggests that biodegradation in the core zone was limited by the availability of oxidants. In lateral zones of the source area, however, gradually more oxidized conditions were reestablished again, suggesting that PHC availability increasingly limited biodegradation. The total DIC production rate in the aquifer decreased within 2 years to about 25% of that during engineered in situ bioremediation and remained at that level. Stable carbon isotope analysis confirmed that the produced DIC mainly originated from PHC mineralization. The total rate of DIC and CH production in the source area was more than 300 times larger than the rate of PHC elution. This indicates that biodegradation coupled to consumption of naturally occurring oxidants was an important process for removal of PHC which remained in the aquifer after terminating engineered measures.
机译:通过注入充气地下水,补充KNO和NHHPO来刺激瑞士Menziken的被柴油污染的含水层,治疗4.5年,以刺激土著居民降解石油烃(PHC)的微生物。在溶解的PHC浓度稳定在较低水平后,终止原位生物修复工程。这项研究的主要目的是评估固有原位生物修复的功效,作为在终止工程原位生物修复后去除含水层中残留PHC的后续措施。在固有的原位生物修复的头7个月中,源区域的氧化还原条件变得更加减轻,这表现为较低浓度的SO 3和较高浓度的Fe(II)和CH。在源区的核心,在剩余的研究期间(3年)中普遍存在严重减少的条件,并且溶解的PHC浓度高于工程原位生物修复过程中的水平。这表明核心区域的生物降解受到氧化剂可用性的限制。然而,在源区的横向区域中,逐渐再次建立了更多的氧化条件,这表明PHC的可用性日益限制了生物降解。含水层中DIC的总生产率在2年内下降到原位生物修复过程中的约25%,并保持在该水平。稳定的碳同位素分析证实,所产生的DIC主要来自PHC矿化。源区域中DIC和CH的总生产速率是PHC洗脱速率的300倍以上。这表明生物降解与消耗天然氧化剂相结合是去除PHC的重要过程,PHC在终止工程措施后仍保留在含水层中。

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