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Is biochar a source or sink for polycyclic aromatic hydrocarbon (PAH) compounds in agricultural soils?

机译:生物炭是否是农业土壤中多环芳烃(PAH)化合物的来源或汇?

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摘要

Polycyclic aromatic hydrocarbons (PAHs) in the environment originate mainly from incomplete combustion of fossil fuels, and pose a significant human health risk. Soils act as environmental sinks for PAHs, as they become strongly absorbed onto soil particles; degradation is mainly driven by microbial catabolism, although it is dependent on PAH bioavailability. There is current interest in burying biochar in soil as a long-term soil carbon store; however, biochar inherently contains varying levels of PAHs and its application could contaminate soil, and its high sorptive capacity may facilitate the persistence of PAHs in the environment. The aim of this study was to determine the effect of adding biochar to soil on microbial mineralization of PAHs, and to quantify whether or not soils amended with biochar were less likely to leach PAHs. We used contrasting agricultural soils (Eutric Cambisol and Cambic Podzol) spiked with the labelled PAH compound 14C-phenanthrene and amended with either wood biochar or rice husk biochar. Mineralization was quantified by measuring the release of 14CO2 and simulated rain used to quantify leaching of PAH through biochar-amended soil. Rice husk biochar had higher concentrations of PAHs (64.65 mg kg-1) than wood biochar (9.56 mg kg-1), and both soil types contained quantifiable levels of PAHs. However, soil that had contained biochar for 3 years had significantly higher levels of PAH (1.95 mg kg-1) compared to unamended soil (1.13 mg kg-1). PAH catabolism in soil was reduced when amended with biochar, although biochar amendment did not consistently decrease PAH leaching. Biochar-mediated inhibition of PAH mineralization is a consequence of increased sorption and reduced bioavailability. Before large scale biochar addition to soils is adopted, future work is needed to address the dynamic between sorbent saturation and microbial activity and how this relates to the concentration of PAHs in soil solution and their persistence in the environment.
机译:环境中的多环芳烃(PAH)主要源自化石燃料的不完全燃烧,对人类健康构成重大威胁。土壤会被PAH强烈吸收,成为PAHs的环境汇聚区。降解主要由微生物分解代谢驱动,尽管它取决于PAH的生物利用度。目前有兴趣将生物炭埋在土壤中作为土壤的长期碳储藏;然而,生物炭固有地含有不同含量的多环芳烃,其应用可能污染土壤,其高吸附能力可能促进多环芳烃在环境中的持久性。这项研究的目的是确定向土壤中添加生物炭对PAHs微生物矿化的影响,并量化用生物炭改性的土壤是否不太可能浸出PAHs。我们使用了对比鲜明的农业土壤(Eutric Cambisol和Cambic Podzol),掺入了标记的PAH化合物14C-菲,并用木材生物炭或稻壳生物炭进行了改良。通过测量14CO2的释放量来量化矿化作用,并使用模拟降雨来量化通过生物炭改良过的土壤中PAH的淋溶。稻壳生物炭中PAHs(64.65 mg kg-1)的浓度高于木材生物炭(9.56 mg kg-1),并且两种土壤类型均含有可定量的PAHs。然而,与未改良的土壤(1.13 mg kg-1)相比,含有生物炭3年的土壤的PAH水平(1.95 mg kg-1)明显更高。尽管生物炭改良剂并不能持续减少PAH的浸出,但当用生物炭进行改良时,土壤中的PAH分解代谢降低了。生物炭介导的PAH矿化抑制是吸附增加和生物利用度降低的结果。在采用向土壤中大量添加生物炭之前,需要做进一步的工作来解决吸附剂饱和度与微生物活性之间的动态关系,以及这与土壤溶液中PAHs的浓度及其在环境中的持久性之间的关系。

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