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老化土壤中石油烃类物质泥浆生物降解过程中生物可利用性限制的评估

Assessment of bioavailability limitations during slurry biodegradation of petroleum hydrocarbons in aged soils.

作者信息

Huesemann Michael H, Hausmann Tom S, Fortman Tim J

机构信息

Battelle Marine Sciences Laboratory, 1529 West Sequim Bay Road, Sequim, Washington 98382, USA.

出版信息

Environ Toxicol Chem. 2003 Dec;22(12):2853-60. doi: 10.1897/02-611.

Abstract

In an effort to determine whether bioavailability limitations are responsible for the slow or incomplete hydrocarbon biodegradation in aged soils, both the rate of desorption (rdes) and biodegradation (rbio) was measured for n-alkanes and polynuclear aromatic hydrocarbons (PAHs) at different times during the slurry biotreatment of six different soils. While all n-alkanes were biodegraded to various degrees depending on their respective carbon number and the soil organic matter content, none of them were desorbed to a significant extent, indicating that these saturated hydrocarbons do not need to be transferred from the soil particles into the aqueous phase in order to be metabolized by microorganisms. Most two- and three-ring PAHs biodegraded as fast as they were desorbed (rbio = rdes); that is, desorption rates controlled biodegradation rates. By contrast, the biodegradation kinetics of four-, five-, and six-ring PAHs was limited by microbial factors during the initial phase (rbio < rdes) while becoming mass-transfer rate limited during the final phase of bioremediation treatment (rbio = rdes). Whenever PAH biodegradation stalled or did not occur at all (rbio = 0), it was never due to bioavailability limitations (rdes >> 0) but was more likely caused by microbial factors. such as the absence of specific PAH degraders or cometabolic substrates. Consequently, PAHs that are found to be microbially recalcitrant in aged soils may not be so because of limited bioavailability and thus could pose a greater risk to the environment than previously thought.

摘要

为了确定生物可利用性限制是否是老化土壤中碳氢化合物生物降解缓慢或不完全的原因,在对六种不同土壤进行泥浆生物处理的不同时间,测量了正构烷烃和多环芳烃(PAHs)的解吸速率(rdes)和生物降解速率(rbio)。虽然所有正构烷烃都根据其各自的碳原子数和土壤有机质含量进行了不同程度的生物降解,但它们都没有大量解吸,这表明这些饱和烃不需要从土壤颗粒转移到水相中就能被微生物代谢。大多数二环和三环多环芳烃的生物降解速率和解吸速率一样快(rbio = rdes);也就是说,解吸速率控制着生物降解速率。相比之下,四环、五环和六环多环芳烃在初始阶段的生物降解动力学受微生物因素限制(rbio < rdes),而在生物修复处理的最后阶段则受传质速率限制(rbio = rdes)。每当多环芳烃生物降解停滞或根本不发生(rbio = 0)时,从来不是由于生物可利用性限制(rdes >> 0),而更可能是由微生物因素引起的。例如缺乏特定的多环芳烃降解菌或共代谢底物。因此,在老化土壤中被发现具有微生物难降解性的多环芳烃,可能并非因为生物可利用性有限,因此可能对环境构成比以前认为的更大风险。

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