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首页> 外文期刊>Journal of Contaminant Hydrology >Analysis of anaerobic BTX biodegradation in a subarctic aquifer using isotopes and benzylsuccinates
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Analysis of anaerobic BTX biodegradation in a subarctic aquifer using isotopes and benzylsuccinates

机译:使用同位素和琥珀酸苄酯分析弧形含水层中厌氧性BTX的生物降解

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In situ biodegradation of benzene, toluene, and xylenes in a petroleum hydrocarbon contaminated aquifer near Fairbanks, Alaska was assessed using carbon and hydrogen compound specific isotope analysis (CSIA) of benzene and toluene and analysis of signature metabolites for toluene (benzylsuccinate) and xylenes (methylbenzylsuccinates). Carbon and hydrogen isotope ratios of benzene were between -25.9 per thousand and -26.8 per thousand for δ~(13)C and -119 per thousand and -136 per thousand for 膥2H, suggesting that biodegradation of benzene is unlikely at this site. However, biodegradation of both xylenes and toluene were documented in this subarctic aquifer. Biodegradation of xylenes was indicated by the presence of methylbenzylsuccinates with concentrations of 17-50 μg/L in three wells. Anaerobic toluene biodegradation was also indicated by benzylsuccinate concentrations of 10-49 μg/L in the three wells with the highest toluene concentrations (1500-5000 μg/L toluene). Since benzylsuccinate typically accounts for a very small fraction of the toluene present in groundwater (generally < 1 mol%), the signature metabolite approach works best at higher toluene concentrations when it is not constrained by detection limits. In wells with lower toluene concentrations (410-640 μg/L), carbon and hydrogen isotopic values were enriched by up to ~2 per thousand for δ~(13)C and ~70 per thousand for δ~2H. This evidence of isotopic fractionation verifies the effects of biodegradation in these low concentration wells where metabolites may already be below detection limits. The combined use of signature metabolite and CSIA data is particularly valuable given the challenge of verifying biodegradation in subarctic environments where degradation rates are typically much slower than in temperate environments.
机译:在费尔班克斯附近的石油烃污染的含水层中对苯,甲苯和二甲苯进行原位生物降解,使用苯和甲苯的碳氢化合物特异性同位素分析(CSIA)以及甲苯(苄基琥珀酸酯)和二甲苯(甲基苄基琥珀酸酯)。对于δ〜(13)C,苯的碳氢同位素比率在-25.9 /-26.8之间,对于膥2H而言,苯的碳和氢同位素比率在-119 /千之间和-136 /千之间,这表明该位置不太可能发生苯的生物降解。 。但是,在该亚弧含水层中记录了二甲苯和甲苯的生物降解。在三个孔中存在浓度为17-50μg/ L的甲基苄基琥珀酸酯表明了二甲苯的生物降解。在甲苯浓度最高的三个孔中(甲苯浓度为1500-5000μg/ L),琥珀酸苄酯的浓度为10-49μg/ L,也表明厌氧甲苯生物降解。由于琥珀酸苄酯通常占地下水中甲苯的极小部分(通常<1 mol%),因此当不受检测极限的限制时,特征代谢物方法在较高的甲苯浓度下效果最佳。在甲苯浓度较低(410-640μg/ L)的井中,δ〜(13)C的碳和氢同位素值富集量高达〜千分之二,δ〜2H的富集度高达〜千分之七十。同位素分馏的证据证明了这些低浓度孔中代谢物可能已经低于检测极限的生物降解作用。考虑到在亚北极环境中验证生物降解的挑战,而降解速度通常比在温带环境中慢得多,因此签名代谢物和CSIA数据的组合使用特别有价值。

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