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Impact of digestate and its fractions on mineralization of ~(14)C-phenanthrene in aged soil

机译:消化物的影响及其馏分对叶片土壤中〜(14)C-菲矿的矿化

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The impact of whole digestate (WD) and its fractions (solid [SD] and liquid [LD]) on C-14-phenanthrene mineralization in soil over 90 d contact time was investigated. The C-14-phenanthrene spiked soil was aged for 1, 30, 60 and 90 d. Analysis of water-soluble nitrogen, phosphorus, total (organic and inorganic) carbon, and quantitative bacterial count were conducted at each time point to assess their impact on mineralization of C-14-phenanthrene in soils. Indigenous catabolic activity (total extents, maximum rates and lag phases) of C-14-phenanthrene mineralization were measured using respirometric soil slurry assay. The soil amended with WD outperformed the SD and LD fractions as well as showed a shorter lag phase, higher rate and extent of mineralization throughout the study. The digestates improved (P 0.05) the microbial population and nutritive content of the soil. However, findings showed that spiking soil with phenanthrene generally reduced the growth of microbial populations from 1 to 90 d and gave a lower nutritive content in comparison with the non-spiked soil. Also, soil fertility and bacteria count were major factors driving C-14-phenanthrene mineralization. Particularly, the non-phenanthrene degraders positively influenced the cumulative mineralization of C-14-phenanthrene after 60 d incubation. Therefore, the digestates (residue from anaerobic digestion) especially WD, which enhanced C-14-phenanthrene mineralization of the soil without minimal basal salts medium nor additional degraders should be further exploited for sustainable bioremediation of PAHs contaminated soil.
机译:研究了全消化(WD)及其级分(固体[SD]和液体[LD])对90d接触时间的C-14菲矿化的影响(固体[Sd]和液体[LD])。 C-14菲掺入的土壤为1,30,60和90d。对水溶性氮,磷,总(有机和无机)碳的分析,以及每次点进行定量细菌计数,以评估它们对土壤中C-14菲矿的影响。使用呼吸泥浆浆料测定测量C-14-菲矿化的土着分解代谢活性(总延伸率,最大率和滞后相)。随着WD修正的土壤优于SD和LD级分,并且在整个研究中显示出较短的滞后阶段,更高的矿化程度和矿化程度。消化物改善(P <0.05)土壤的微生物种群和营养含量。然而,结果表明,尖峰土壤与菲苯丙烯通常会降低1至90d的微生物群的生长,并与非尖刺土相比,较低的营养含量。此外,土壤肥力和细菌数量是推动C-14菲矿化的主要因素。特别是,非菲苯乙烯降解率为60d孵育后呈正影响C-14菲酸的累积矿化。因此,尤其是Wd的消化(来自厌氧消化的残留物),其增强了没有最小基础盐培养基的土壤C-14菲矿化,也应进一步利用PAHS受污染土壤的可持续生物修复。

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