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Biochar in Co-Contaminated Soil Manipulates Arsenic Solubility and Microbiological Community Structure and Promotes Organochlorine Degradation

机译:共污染土壤中的生物碳操纵砷的溶解度和微生物群落结构并促进有机氯的降解

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摘要

We examined the effect of biochar on the water-soluble arsenic (As) concentration and the extent of organochlorine degradation in a co-contaminated historic sheep-dip soil during a 180-d glasshouse incubation experiment. Soil microbial activity, bacterial community and structure diversity were also investigated. Biochar made from willow feedstock (Salix sp) was pyrolysed at 350 or 550°C and added to soil at rates of 10 g kg-1 and 20 g kg-1 (representing 30 t ha-1 and 60 t ha-1). The isomers of hexachlorocyclohexane (HCH) alpha-HCH and gamma-HCH (lindane), underwent 10-fold and 4-fold reductions in concentration as a function of biochar treatment. Biochar also resulted in a significant reduction in soil DDT levels (P < 0.01), and increased the DDE:DDT ratio. Soil microbial activity was significantly increased (P < 0.01) under all biochar treatments after 60 days of treatment compared to the control. 16S amplicon sequencing revealed that biochar-amended soil contained more members of the Chryseobacterium, Flavobacterium, Dyadobacter and Pseudomonadaceae which are known bioremediators of hydrocarbons. We hypothesise that a recorded short-term reduction in the soluble As concentration due to biochar amendment allowed native soil microbial communities to overcome As-related stress. We propose that increased microbiological activity (dehydrogenase activity) due to biochar amendment was responsible for enhanced degradation of organochlorines in the soil. Biochar therefore partially overcame the co-contaminant effect of As, allowing for enhanced natural attenuation of organochlorines in soil.
机译:在180天的温室孵化实验中,我们研究了生物炭对水溶性砷(As)浓度和有机污染的历史悠久的绵羊浸入土壤中有机氯降解程度的影响。还调查了土壤微生物活性,细菌群落和结构多样性。将柳树原料(Salix sp)制成的生物炭在350或550°C下热解,并以10 g kg -1 和20 g kg -1 (代表30 t ha -1 和60 t ha -1 )。六氯环己烷(HCH)α-HCH和γ-HCH(林丹)的异构体的浓度随生物炭处理而降低了10倍和4倍。生物炭还导致土壤滴滴涕水平显着降低(P <0.01),并增加了滴滴涕:滴滴涕的比率。与对照相比,在所有生物炭处理后60天,土壤微生物活性均显着增加(P <0.01)。 16S扩增子测序表明,经生物炭修饰的土壤含有更多的金黄色葡萄球菌,黄杆菌,双歧杆菌和假单胞菌科成员,它们是已知的碳氢化合物生物修复剂。我们假设由于生物炭的改良而导致的可溶砷浓度的短期减少使本地土壤微生物群落能够克服与砷相关的胁迫。我们建议由于生物炭的改良而增加的微生物活性(脱氢酶活性)是造成土壤中有机氯降解增强的原因。因此,生物炭部分克服了砷的共污染作用,从而增强了土壤中有机氯的自然衰减。

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