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生物强化对原始土壤和污染土壤中微生物迁移、水分入渗、水分损失及表面硬度的影响。

Effect of bioaugmentation on microbial transport, water infiltration, moisture loss, and surface hardness in pristine and contaminated soils.

作者信息

Mehmannavaz R, Prasher S O, Ahmad D

机构信息

INRS-Institut Armand-Frappier, Centre de microbiologie et biotechnologie, 245 boulevard Hymus, Pointe-Claire, Québec, H9R 1G6, Canada.

出版信息

J Environ Sci Health A Tox Hazard Subst Environ Eng. 2001;36(2):123-39. doi: 10.1081/ese-100102612.

Abstract

Three different soils, a clay, a pristine sandy loam and a PCB-contaminated sandy loam, were bioaugmented to determine the influence of clay content and contaminants on the transport of bacteria in unsaturated soils, using surface irrigation water as a transport medium. The results indicate that the transport of the implanted bacteria was influenced negatively more by the presence of PCBs than by the clay content of the soil. Transport was directly related to the frequency of irrigation and length of the intervals between irrigation periods, making these variables important factors to consider when applying bioaugmentation via downward percolating water. Other parameters measured after bacterial bioaugmentation were water infiltration, moisture loss, and surface hardness of these soils. Surface water infiltration was affected more by the soil clay content than by the hydrophobic contaminant. Infiltration was significantly but differently influenced by bioaugmentation, positively in clay, negatively in sandy loam, and negatively (to a lesser extent) in the PCB-contaminated sandy loam soils. Moisture loss was slower in the bioaugmented soil than in the control soils, with this difference being most pronounced in the PCB soil. High moisture loss in the bioaugmented clay soil rendered it the hardest soil for surface penetration.

摘要

使用地表灌溉水作为传输介质,对三种不同的土壤(一种黏土、一种原始砂壤土和一种多氯联苯污染的砂壤土)进行生物强化,以确定黏土含量和污染物对非饱和土壤中细菌传输的影响。结果表明,与土壤的黏土含量相比,多氯联苯的存在对植入细菌的传输产生的负面影响更大。传输与灌溉频率和灌溉周期之间的间隔长度直接相关,这使得这些变量成为通过向下渗透水进行生物强化时需要考虑的重要因素。在细菌生物强化后测量的其他参数包括这些土壤的水分入渗、水分损失和表面硬度。地表水入渗受土壤黏土含量的影响大于受疏水性污染物的影响。生物强化对入渗有显著但不同的影响,在黏土中为正向影响,在砂壤土中为负向影响,在多氯联苯污染的砂壤土中为负向影响(程度较小)。生物强化土壤中的水分损失比对照土壤中的慢,这种差异在多氯联苯污染土壤中最为明显。生物强化黏土土壤中的高水分损失使其成为表面最难穿透的土壤。

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