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Benzene degradation in contaminated aquifers: Enhancing natural attenuation by injecting nitrate

机译:受污染含水层的苯降解:通过注射硝酸盐来提高自然衰减

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Natural attenuation processes depend on the availability of suitable electron acceptors. At the megasite Zeitz, concentrations of the main contaminant benzene were observed to increase constantly in the lower aquifer to levels of more than 2.5 mM. This was accompanied by decreasing concentrations of sulphate (SO42? ), which has been previously shown to be the main electron acceptor for benzene oxidation at this site, resulting in an electron acceptor-limited, sulphidic benzene plume. Therefore, a field experiment was conducted to stimulate benzene biodegradation by injecting nitrate (NO3? ) into the sulphidic benzene plume aiming (i) to recycle sulphate by nitrate-dependent sulphide oxidation, and (ii) to serve as direct electron acceptor for benzene oxidation. Within 60 days, 6.74 tons sodium nitrate (NaNO3) were injected into the lower aquifer, and the resulting biogeochemical effects within the benzene plume were monitored for more than one year by chemical and microbiological analyses of groundwater samples taken from various depths of ten monitoring wells located in three observation lines downstream of nitrate injection. Nitrate was microbiologically consumed, as shown by changes in 815NNO3? and 818O-NO3? values, partial nitrite accumulation, and changing ratios of Na+/NO3? . Main electron donors for nitrate reduction were reduced sulphur compounds, verified by changing 834S-SO42- and 818O-SO42? values, partially increasing sulphate concentrations, and strongly increasing abundances of typical sulphur-oxidizing, nitrate-reducing bacterial taxa within the nitrate plume. The general absent hydrogen isotope fractionation of benzene, also in the sulphidic, nitrate-free part of the plume, indicates that benzene was not biodegraded by sulphate-reducing consortia. However, detected small carbon isotope fractionation of benzene points to in situ benzene biodegradation processes in the plume, probably supported by nitrate. In conclusion, nitrate injection resulted in changing redox conditions and recycling of sulphate in the sulphidic, sulphate-depleted benzene plume due to microbial oxidation of reduced sulphur species, leading to presumably favored conditions for in situ benzene biodegradation.
机译:自然衰减过程取决于合适的电子受体的可用性。在巨沸石Zeitz,观察到主要污染物苯的浓度在较低含水层中不断增加,达到2.5毫米的水平。这伴随着降低硫酸盐浓度(SO42?)的浓度,该浓度先前被证明是该位点的苯氧化的主要电子受体,导致电子受体限制,硫酸苯羽流。因此,通过将硝酸盐(NO 3→)注入硫酸苯羽流(I)以通过硝酸依赖性硫化物氧化再循环硫酸盐来刺激苯生物降解,以用作苯氧化的直接电子受体以再循环硫酸盐。在60天内,将6.74吨硝酸钠(NANO3)注入较低含水层,通过从10个监测井的各种深度采取的地下水样本进行化学和微生物分析,监测苯羽流内的生物地质化学作用位于硝酸注射下游的三条观察线。硝酸盐是微生物学消耗的,如815nno3的变化所示?和818O-no3? Na + / No3的值,部分亚硝酸盐积累和变化比率? 。用于硝酸盐还原的主电子给体还原硫化合物,通过改变834S-SO42-和818O-SO42来验证?值,部分增加硫酸盐浓度,以及硝酸盐羽流内典型硫氧化,硝酸盐还原的细菌分类群的强烈增加。苯的一般缺乏氢同位素分馏,也在亚硫酸盐,无硝酸盐部分的羽流中表明苯不通过硫酸盐减少的组成生物降解。然而,检测到苯点的小碳同位素分馏在羽流中的原位苯生物降解过程中,可能由硝酸盐支撑。总之,硝酸注射导致氧化还原条件和硫酸盐中硫酸盐的再循环导致硫酸盐的硫酸盐含量的氧化含量降低,导致原位苯生物降解的可能有利于原位的条件。

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