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Microbial community response to a release of neat ethanol onto residual hydrocarbons in a pilot-scale aquifer tank

机译:试点规模的含水层池中微生物对净乙醇释放到残留碳氢化合物上的反应

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The microbial community response to a neat ethanol release (E100, 76 l) onto residual hydrocarbons in sandy soil was evaluated in a continuous-flow 8 m(3) pilot-scale aquifer tank, simulating a release at a bulk fuel terminal. Microbial genotypic shifts were assessed using quantitative real-time PCR analysis. High ethanol concentrations in the capillary fringe at potentially toxic levels, exceeding 100 000 mg l(-1), were tolerated by the microbial community. The high biochemical oxygen demand exerted by ethanol rapidly induced anaerobic conditions, and both methane production (up to 1.2 mg l(-1)) and growth of putative methanogenic Archaea (up to 10(6) gene copies per g of soil) were observed in shallow groundwater and soil samples 75 cm down gradient from the source. Aerobic conditions returned after ethanol was flushed out of the system, approximately 45 days after the spill (less than 7.5 pore volumes flushed). Total Bacteria growth coincided with ethanol migration and availability, which was restricted to a relatively thin layer at the capillary fringe and water table interface. The concentrations of bacteria harbouring the aerobic catabolic genes dmpN (coding for phenol hydroxylase) and todC1 (coding for toluene dioxygenase) increased (up to 100x) down gradient from the source, likely as a result of both fortuitous growth on ethanol and on aromatic hydrocarbons mobilized by ethanol. Growth of hydrocarbon degraders was corroborated by denaturing gradient gel electrophoresis analysis showing proliferation of Azospirillum and Brevundimonas spp., which are bacteria commonly associated with microaerophilic hydrocarbon degradation. Nevertheless, the relative abundance of hydrocarbon-specific degraders (as a fraction of total Bacteria) decreased as other bacteria grew to a higher extent. Overall, the observed growth of hydrocarbon degraders suggests a potential enhancement in aerobic natural attenuation in shallow aquifers after ethanol and its degradation by-products are degraded or flushed from sites impacted by ethanol-blended fuels.
机译:在连续流动的8 m(3)中试规模含水层水箱​​中评估微生物对纯净乙醇释放到沙质土壤中残留碳氢化合物上的纯乙醇释放(E100,76 l)的响应,模拟散装燃料终端的释放。使用定量实时PCR分析评估微生物的基因型变化。微生物群落可耐受毛细边缘中的高浓度乙醇,其潜在毒性水平超过100 000 mg l(-1)。乙醇施加的高生化需氧量迅速诱导了厌氧条件,并观察到甲烷的产生(高达1.2 mg l(-1))和推定的产甲烷古细菌的生长(每克土壤最多10(6)个基因拷贝)在浅层地下水和土壤样品中,从源头向下倾斜75厘米。泄漏后大约45天(将少于7.5的孔体积冲洗掉)后,将乙醇从系统中冲洗掉后,有氧条件又恢复了。细菌总数的增长与乙醇的迁移和可利用性相吻合,乙醇被限制在毛细管边缘和地下水位界面相对较薄的一层。含有好氧分解代谢基因dmpN(编码酚羟化酶)和todC1(编码甲苯双加氧酶)的细菌浓度从源头开始向下梯度增加(最高100倍),这可能是由于乙醇和芳香烃的偶然生长造成的由乙醇调动。通过变性梯度凝胶电泳分析证实了碳氢降解物的生长,变性梯度凝胶电泳分析显示了与微需氧碳氢化合物降解通常相关的细菌-细螺旋藻和短螺旋藻属的繁殖。然而,随着其他细菌的生长,碳氢化合物特异性降解物的相对丰度(占细菌总数的比例)下降。总体而言,观察到的碳氢化合物降解物的生长表明,在乙醇及其降解副产物被乙醇混合燃料影响的地点降解或冲洗后,浅层含水层中有氧自然衰减的潜在增强作用。

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