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首页> 外文期刊>Cold regions science and technology >Hydraulic conductivity change of bio-barrier formed in the subsurface by the adverse conditions including freeze-thaw cycles
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Hydraulic conductivity change of bio-barrier formed in the subsurface by the adverse conditions including freeze-thaw cycles

机译:冻融循环等不利条件在地下形成的生物屏障的水力传导率变化

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摘要

Bio-barrier is an emerging technology to control subsurface contaminant plum by making microorganisms clog soil pore to form a subsurface barrier. Extracellular polymeric substances (EPS) of microorganisms play an important role to maintain decreased hydraulic conductivity; In this research, the hydraulic conductivity changes of biomass-soil mixtures by the adverse conditions were studied to evaluate the applicability to the field condition as an alternative barrier material. The microorganisms used in this research were bacterium, Azotobacter chroococcum, and fungus, Aureobasidium pullulans, respectively. The hydraulic conductivity decreased to 1-10% of the initial hydraulic conductivity of residual soil, 1 x 10~(-4) cm/s, and stayed constant while substrate was provided. Under adverse conditions such as no substrate available, chemical solution permeation and freeze-thaw cycles, the hydraulic conductivity increased by 30-50% compared to the lowest value. The decrease of hydraulic conductivity in a fungus-soil mixture was faster than that of a bacterium-soil mixture. The fungus-soil mixture, however, was more sensitive to the adverse conditions. After the adverse conditions, hydraulic conductivity shows even lower value compare to that of before the adverse conditions.
机译:生物屏障是一种新兴技术,它通过使微生物阻塞土壤孔隙形成地下屏障来控制地下污染物。微生物的细胞外聚合物(EPS)在维持降低的水力传导性方面起着重要作用。在这项研究中,研究了不利条件下生物质-土壤混合物的水力传导率变化,以评估其作为替代阻隔材料在田间条件下的适用性。在这项研究中使用的微生物分别是细菌,绿球菌和真菌,金黄色葡萄球菌。水力传导率下降到残余土壤初始水力传导率的1-10%,为1 x 10〜(-4)cm / s,并在提供基质时保持恒定。在不利条件下,例如无底物可用,化学溶液渗透和冻融循环,与最低值相比,水力传导率增加了30-50%。真菌-土壤混合物中水力传导率的下降速度快于细菌-土壤混合物中水力传导率的下降速度。然而,真菌-土壤混合物对不利条件更为敏感。不利条件之后,水力传导率显示出比不利条件之前更低的值。

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