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Multicycle Ozonation+Bioremediation for Soils Containing Residual Petroleum

机译:含残留石油的土壤的多循环臭氧+生物修复

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We systematically assessed the removal of total petroleum hydrocarbons (TPHs) and other organic carbon using sequential biodegradation and ozonation in two soils (BM3 and BM4). We optimized the conditions for each step: 5% moisture content for ozonation and 10% moisture and circumneutral pH for biodegradation. For the relatively biodegradable TPH in BM3, preozonation and postozonation strategies were equally effective. In contrast, the more recalcitrant TPH in BM4 was better treated using postozonation. Carbon analyses along the treatment timeline revealed that dissolved organic carbon (DOC) was the dominant substrate for microbial consumption when readily biodegradable TPH was no longer available. The carbon in TPH was more reactive with O3 than was the rest of dichloromethane-extractable organic carbon (DeOC), and the fate of TPH dictated the changes of DeOC. However, the fate of total organic carbon was controlled mainly by the microbial mineralization of DOC. Ozonation did not directly enhance the biodegradation rate of the residual TPH after ozonation, but ozone converted TPH into DOC that was microbially mineralized. This is the first study that compares the efficiencies of pre- and postozonation of two distinctly different soils. This study provides insights regarding the fundamental mechanism through which biodegradation and ozonation integrate and reveals the dynamics between ozonation and biodegradation during treatment petroleum-contaminated soils. Multistage ozonation+biodegradation is a useful tool to achieve the regulatory TPH standard (10,000 mg/kg), and DOC should be measured alongside TPH to gauge the dynamics of the integrated process.
机译:我们通过在两种土壤(BM3和BM4)中进行顺序生物降解和臭氧化,系统地评估了总石油烃(TPHs)和其他有机碳的去除。我们优化了每个步骤的条件:5%的水分用于臭氧氧化,10%的水分和环境pH用于生物降解。对于BM3中可生物降解的TPH,预臭氧化和后臭氧化策略同样有效。相反,使用后臭氧处理可以更好地治疗BM4中顽固的TPH。沿处理时间表进行的碳分析显示,当不再存在可生物降解的TPH时,溶解的有机碳(DOC)是微生物消耗的主要底物。 TPH中的碳与O3的反应性比其余的可通过二氯甲烷萃取的有机碳(DeOC)更高,TPH的命运决定了DeOC的变化。然而,总有机碳的命运主要受DOC的微生物矿化控制。臭氧化并没有直接提高臭氧化后残留TPH的生物降解率,但臭氧将TPH转化为微生物矿化的DOC。这是第一项比较两种截然不同的土壤的臭氧化前和臭氧后效率的研究。这项研究提供了有关生物降解和臭氧化作用整合的基本机理的见解,并揭示了在石油污染土壤的处理过程中,臭氧化作用和生物降解之间的动力学关系。多级臭氧氧化+生物降解是达到监管的TPH标准(10,000 mg / kg)的有用工具,应与TPH一起测量DOC,以评估集成过程的动力学。

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