Cápiro Natalie L, Da Silva Marcio L B, Stafford Brent P, Rixey William G, Alvarez Pedro J J
Department of Civil and Environmental Engineering, Rice University, 6100 Main Street - MS 317, Houston, TX 77005, USA.
Environ Microbiol. 2008 Sep;10(9):2236-44. doi: 10.1111/j.1462-2920.2008.01645.x. Epub 2008 May 14.
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 to dC1 (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.
在一个8立方米的中试规模连续流含水层试验槽中,模拟散装燃料码头的泄漏情况,评估了微生物群落对向沙质土壤中的残留烃释放纯乙醇(E100,76升)的响应。使用定量实时PCR分析评估微生物基因型变化。微生物群落能够耐受毛细边缘处潜在有毒水平的高乙醇浓度,超过100,000毫克/升。乙醇产生的高生化需氧量迅速诱导了厌氧条件,在距源头下游75厘米处的浅层地下水和土壤样品中观察到甲烷生成(高达1.2毫克/升)以及假定产甲烷古菌的生长(高达每克土壤10⁶个基因拷贝)。乙醇从系统中被冲洗出去后,有氧条件恢复,泄漏后约45天(冲洗的孔隙体积小于7.5倍)。总细菌生长与乙醇的迁移和可用性一致,乙醇的迁移和可用性仅限于毛细边缘和地下水位界面处相对较薄的一层。携带需氧分解代谢基因dmpN(编码苯酚羟化酶)和to dC1(编码甲苯双加氧酶)的细菌浓度从源头向下游梯度增加(高达100倍),这可能是由于偶然在乙醇上生长以及在乙醇动员的芳香烃上生长的结果。变性梯度凝胶电泳分析证实了烃降解菌的生长,显示出固氮螺菌属和短波单胞菌属的增殖,这些细菌通常与微需氧烃降解有关。然而,随着其他细菌生长到更高程度,烃特异性降解菌的相对丰度(占总细菌的比例)下降。总体而言,观察到的烃降解菌生长表明,在乙醇及其降解副产物从受乙醇混合燃料影响的场地降解或冲洗后,浅层含水层中的需氧自然衰减可能会增强。