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Distribution and location of polycyclic aromatic hydrocarbons (PAHs) andPAH-degrading bacteria within polluted soil aggregates

机译:多环芳烃(PAHs)和降解PAH的细菌在污染土壤团聚体中的分布和位置

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A study was conducted to determine the location and distribution of PAH and PAH-degrading bacteria in different aggregate size fractions of an industrially polluted soil. The estimation of PAH-degrading bacteria using an MPN microplate technique indicated that these bacteria are most numerous in the aggregate size fractions corresponding to fine silt (2-20 mum) and clay (<2 mum) compared to larger fractions or unfractionated soil. PAH concentrations were also highest in the aggregate size fraction corresponding to fine silt. Similar results were found in a spiked soil (incubated for 6 months) with similar carbonated minerals. Transmission electron microscopy observations showed that the autochtonous PAH-degrading bacteria were embedded in the aggregates where PAHs were abundant. In spite of this extensive co-localisation PAH degradation was limited during 6 months incubation. This indicates that factors other than spatial distribution and PAH degrading ability control degradation rates. The fine silt fraction of the industrial soil had an elevated C/N ratio (35) compared to the clay fraction (C/N: 16). Thus the fraction which assumably had the highest specific surface area contained less PAH but similar numbers of PAH-degraders. N thus seem to play an important role in the long term, but as PAH degradation was low in fine size fractions, other sources/factors were probably limiting (easily degradable C, P org, O-2 etc.). Based on these findings, soil particle organization and structure of soil aggregates appear to be important for the characterization of a polluted soil (localization and sequestration). Manipulations that modify aggregation in polluted soils could thus potentially influence the accessibility and biodegradability of PAHs.
机译:进行了一项研究,以确定工业污染土壤中不同聚集体级分中PAH和降解PAH的细菌的位置和分布。使用MPN微孔板技术对降解PAH的细菌进行的估算表明,与较大级分或未分级土壤相比,这些细菌的团粒大小分数最多,相当于细粉砂(2-20 mum)和黏土(<2 mum)。 PAH浓度在对应于细粉砂的骨料中也最高。在掺有类似碳酸矿物质的掺加土壤(孵育6个月)中发现了相似的结果。透射电子显微镜观察表明,降解PAH的自生细菌被埋在富含PAH的聚集体中。尽管进行了广泛的共定位,但在6个月的孵育过程中,PAH的降解仍然受到限制。这表明除空间分布和PAH降解能力以外的其他因素可控制降解速率。与粘土部分(C / N:16)相比,工业土壤的细粉土部分具有更高的C / N比(35)。因此,推测具有最高比表面积的级分含有较少的PAH,但PAH降解剂的数目相似。因此,从长远来看,N似乎起着重要的作用,但是由于PAH的降解程度很小,因此其他来源/因素可能会受到限制(容易降解的C,Porg,O-2等)。基于这些发现,土壤颗粒的组织和土壤团聚体的结构对于表征污染土壤(定位和固结)似乎很重要。因此,改变污染土壤中聚集的操作可能会影响PAHs的可及性和生物降解性。

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