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挪威和英国“原始”林地和草地土壤中土著 C-菲的生物降解。

Indigenous C-phenanthrene biodegradation in "pristine" woodland and grassland soils from Norway and the United Kingdom.

机构信息

University of Derby, UK.

出版信息

Environ Sci Process Impacts. 2017 Nov 15;19(11):1437-1444. doi: 10.1039/c7em00242d.

Abstract

In this study, the indigenous microbial mineralisation of C-phenanthrene in seven background soils (four from Norwegian woodland and three from the UK (two grasslands and one woodland)) was investigated. ∑PAHs ranged from 16.39 to 285.54 ng g dw soil. Lag phases (time before C-phenanthrene mineralisation reached 5%) were longer in all of the Norwegian soils and correlated positively with TOC, but negatively with ∑PAHs and phenanthrene degraders for all soils. C-phenanthrene mineralisation in the soils varied due to physicochemical properties. The results show that indigenous microorganisms can adapt to C-phenanthrene mineralisation following diffuse PAH contamination. Considering the potential of soil as a secondary PAH source, these findings highlight the important role of indigenous microflora in the processing of PAHs in the environment.

摘要

本研究调查了七种背景土壤(挪威林地土壤 4 种,英国草地和林地土壤各 3 种)中 C-菲的土著微生物矿化作用。∑PAHs 范围为 16.39 至 285.54ng g dw 土壤。所有挪威土壤的滞后期(C-菲矿化达到 5%之前的时间)都更长,与 TOC 呈正相关,但与所有土壤的∑PAHs 和菲降解菌呈负相关。土壤中 C-菲的矿化因理化性质而异。结果表明,土著微生物可以在多环芳烃污染后适应 C-菲的矿化作用。考虑到土壤作为二次 PAH 源的潜力,这些发现强调了土著微生物群在环境中 PAHs 处理中的重要作用。

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