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Typical Soil Redox Processes in Pentachlorophenol Polluted Soil Following Biochar Addition

机译:添加生物炭后五氯苯酚污染土壤的典型土壤氧化还原过程

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摘要

Reductive dechlorination is the primary pathway for environmental removal of pentachlorophenol (PCP) in soil under anaerobic condition. This process has been verified to be coupled with other soil redox processes of typical biogenic elements such as carbon, iron and sulfur. Meanwhile, biochar has received increasing interest in its potential for remediation of contaminated soil, with the effect seldom investigated under anaerobic environment. In this study, a 120-day anaerobic incubation experiment was conducted to investigate the effects of biochar on soil redox processes and thereby the reductive dechlorination of PCP under anaerobic condition. Biochar addition (1%, w/w) enhanced the dissimilatory iron reduction and sulfate reduction while simultaneously decreased the PCP reduction significantly. Instead, the production of methane was not affected by biochar. Interestingly, however, PCP reduction was promoted by biochar when microbial sulfate reduction was suppressed by addition of typical inhibitor molybdate. Together with Illumina sequencing data regarding analysis of soil bacteria and archaea responses, our results suggest that under anaerobic condition, the main competition mechanisms of these typical soil redox processes on the reductive dechlorination of PCP may be different in the presence of biochar. In particularly, the effect of biochar on sulfate reduction process is mainly through promoting the growth of sulfate reducer (Desulfobulbaceae and Desulfobacteraceae) but not as an electron shuttle. With the supplementary addition of molybdate, biochar application is suggested as an improved strategy for a better remediation results by coordinating the interaction between dechlorination and its coupled soil redox processes, with minimum production of toxic sulfur reducing substances and relatively small emission of greenhouse gas (CH4) while maximum removal of PCP.
机译:还原性脱氯是在厌氧条件下去除土壤中五氯苯酚(PCP)的主要途径。该过程已被证实与其他典型生物元素如碳,铁和硫的土壤氧化还原过程结合在一起。同时,生物炭对其被污染土壤的修复潜力越来越感兴趣,在厌氧环境下很少研究其效果。在这项研究中,进行了为期120天的厌氧培养实验,以研究生物炭对土壤氧化还原过程的影响,从而研究PCP在厌氧条件下的还原性脱氯作用。添加生物炭(1%,w / w)增强了异化铁的还原和硫酸盐的还原,同时显着降低了PCP的还原。相反,甲烷的生产不受生物炭的影响。然而,有趣的是,当通过添加典型的抑制剂钼酸盐来抑制微生物硫酸盐还原时,生物炭促进了PCP还原。结合有关土壤细菌和古细菌响应分析的Illumina测序数据,我们的结果表明,在无氧条件下,这些典型的土壤氧化还原过程对PCP还原脱氯的主要竞争机制在存在生物炭的情况下可能有所不同。特别是,生物炭对硫酸盐还原过程的影响主要是通过促进硫酸盐还原剂(脱硫鳞茎科和脱硫细菌科)的生长,而不是通过电子穿梭。在补充钼酸盐的情况下,建议通过协调脱氯与其耦合的土壤氧化还原过程之间的相互作用,减少有毒的硫还原物质的产生以及减少温室气体(CH4)的排放,来应用生物炭作为改善补救效果的改进策略。 ),同时最大程度地去除PCP。

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