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在硫酸盐还原条件下,含水层微生物对甲苯和二甲苯的厌氧降解。

Anaerobic degradation of toluene and xylene by aquifer microorganisms under sulfate-reducing conditions.

作者信息

Edwards E A, Wills L E, Reinhard M, Grbić-Galić D

机构信息

Department of Civil Engineering, Stanford University, California 94305-4020.

出版信息

Appl Environ Microbiol. 1992 Mar;58(3):794-800. doi: 10.1128/aem.58.3.794-800.1992.

Abstract

Toluene and the three isomers of xylene were completely mineralized to CO2 and biomass by aquifer-derived microorganisms under strictly anaerobic conditions. The source of the inoculum was gasoline-contaminated sediment from Seal Beach, Calif. Evidence confirming that sulfate was the terminal electron acceptor is presented. Benzene and ethylbenzene were not degraded under the experimental conditions used. Successive transfers of the mixed cultures that were enriched from aquifer sediments retained the ability to degrade toluene and xylenes. Greater than 90% of 14C-labeled toluene or 14C-labeled o-xylene was mineralized to 14CO2. The doubling time for the culture grown on toluene or m-xylene was about 20 days, and the cell yield was about 0.1 to 0.14 g of cells (dry weight) per g of substrate. The accumulation of sulfide in the cultures as a result of sulfate reduction appeared to inhibit degradation of aromatic hydrocarbons.

摘要

在严格厌氧条件下,含水层中的微生物可将甲苯和二甲苯的三种异构体完全矿化生成二氧化碳和生物质。接种物来源于加利福尼亚州海豹滩受汽油污染的沉积物。文中提供了证实硫酸盐是末端电子受体的证据。在所用实验条件下,苯和乙苯未被降解。从含水层沉积物中富集得到的混合培养物经连续传代后,仍保留降解甲苯和二甲苯的能力。超过90%的14C标记甲苯或14C标记邻二甲苯被矿化生成14CO2。以甲苯或间二甲苯为底物生长的培养物的倍增时间约为20天,细胞产量约为每克底物产生0.1至0.14克细胞(干重)。由于硫酸盐还原导致培养物中硫化物的积累,似乎抑制了芳烃的降解。

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