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首页> 外文期刊>Journal of Contaminant Hydrology >Migration and natural fate of a coal tar creosote plume 2. Mass balance and biodegradation indicators
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Migration and natural fate of a coal tar creosote plume 2. Mass balance and biodegradation indicators

机译:煤焦油杂酚羽的迁移和自然命运2.质量平衡和生物降解指标

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A source of coal tar creosote was emplaced below the water table at CFB Borden to investigate natural attenuation processes for complex biodegradable mixtures. A mass balance indicated that ongoing transformation occurred for seven study compounds. Phenol migrated as a discrete slug plume and almost completely disappeared after 2 years, after being completely leached from the source early in the study. The m-xylene plume migrated outward to a maximum distance at approximately 2 years, and then receded back towards the source as the rate of mass flux out of the source decreased to below the overall rate of plume transformation. Carbazole showed similar behaviour, although the reversal in plume development occurred more slowly. The dibenzofuran plume remained relatively constant in extent and mass over the last 2 years of monitoring, despite constant source input over this period, providing evidence that the dibenzofuran plume was at steady state. Meanwhile, the naphthalene and 1-methylnaphthalene plumes continued to advance and increase in mass over the observation period, although at a decreasing rate. The phenanthrene plume was also subject to transformation, although measurement of the rate was less conclusive due to the higher proportion of sorbed mass for this compound. Three lines of evidence are presented to evaluate whether the observed plume mass loss was due to microbial biodegradation. Measurement of redox--sensitive parameters in the vicinity of the plume showed the types of changes that would be expected to occur due to plume biodegradation; dissolved oxygen and SO_4~2- decreased in groundwater within the plume while significant increases were noted for Fe'+, Mn~2+ and methane. Further evidence that plume mass loss was microbially-mediated was provided by the accumulation of aromatic acids within the plume. Measurements of phospholipid fatty acids (PLFA) in aquifer material indicated that microbial biomass and turnover rate were greater within the plume than outside f also consistent with biodegradation. Study results highlight the potential for utilizing natural attenuation as a site cleanup approach for dissolved phase plumes from complex organic mixture like coal tar creosote.
机译:CFB Borden的地下水位以下放置了煤焦油杂酚油,以研究复杂的可生物降解混合物的自然衰减过程。质量平衡表明,七个研究化合物正在进行转化。在研究初期从源中完全浸出后,苯酚以不连续的毛羽形式迁移,并在2年后几乎完全消失。间二甲苯羽流向外迁移到最大距离大约为2年,然后随着从源中流出的质量通量的比率降低到羽流转化的总速率以下而退回到源。咔唑表现出相似的行为,尽管羽流发展的逆转发生的速度较慢。尽管在此期间源源不断输入,但在过去两年的监测中,二苯并呋喃羽流的范围和质量仍保持相对恒定,这提供了二苯并呋喃羽流处于稳定状态的证据。同时,在观察期间,萘和1-甲基萘的羽流继续前进并质量增加,尽管速率降低。菲羽也经历了转化,尽管由于该化合物的吸附质量比例较高,所以速率的测定尚无定论。提供了三行证据来评估观察到的羽流质量损失是否是由于微生物的生物降解所致。在羽流附近对氧化还原敏感参数的测量显示了由于羽流生物降解而可能发生的变化类型。羽状流中地下水中的溶解氧和SO_4〜2-减少,而Fe'+,Mn〜2 +和甲烷则显着增加。羽状物质质量损失是由微生物介导的,这是由羽状物质中芳香酸的积累提供的。对含水层材料中磷脂脂肪酸(PLFA)的测量表明,羽状流中微生物的生物量和周转率大于外部羽状流,这也与生物降解相符。研究结果突显了利用自然衰减作为现场清理方法处理来自复杂有机混合物(如煤焦油杂酚)的溶解相羽流的潜力。

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