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运动性脱氯地杆菌迁移至三氯乙烯致密非水相液体的模型源区:实验评估与建模

Motile Geobacter dechlorinators migrate into a model source zone of trichloroethene dense non-aqueous phase liquid: experimental evaluation and modeling.

作者信息

Philips Jo, Miroshnikov Alexey, Haest Pieter Jan, Springael Dirk, Smolders Erik

机构信息

Department of Earth and Environmental Sciences, Division of Soil and Water Management, KU Leuven (University of Leuven), Kasteelpark Arenberg 20, B-3001 Heverlee, Belgium.

Department of Mathematics and Statistics, University of Massachusetts, Lederle Graduate Research Tower, Amherst MA 01003-9305, USA.

出版信息

J Contam Hydrol. 2014 Dec 1;170:28-38. doi: 10.1016/j.jconhyd.2014.09.010. Epub 2014 Oct 2.

Abstract

Microbial migration towards a trichloroethene (TCE) dense non-aqueous phase liquid (DNAPL) could facilitate the bioaugmentation of TCE DNAPL source zones. This study characterized the motility of the Geobacter dechlorinators in a TCE to cis-dichloroethene dechlorinating KB-1(™) subculture. No chemotaxis towards or away from TCE was found using an agarose in-plug bridge method. A second experiment placed an inoculated aqueous layer on top of a sterile sand layer and showed that Geobacter migrated several centimeters in the sand layer in just 7days. A random motility coefficient for Geobacter in water of 0.24±0.02cm(2)·day(-1) was fitted. A third experiment used a diffusion-cell setup with a 5.5cm central sand layer separating a DNAPL from an aqueous top layer as a model source zone to examine the effect of random motility on TCE DNAPL dissolution. With top layer inoculation, Geobacter quickly colonized the sand layer, thereby enhancing the initial TCE DNAPL dissolution flux. After 19days, the DNAPL dissolution enhancement was only 24% lower than with an homogenous inoculation of the sand layer. A diffusion-motility model was developed to describe dechlorination and migration in the diffusion-cells. This model suggested that the fast colonization of the sand layer by Geobacter was due to the combination of random motility and growth on TCE.

摘要

微生物向三氯乙烯(TCE)致密非水相液体(DNAPL)迁移可促进TCE DNAPL源区的生物强化。本研究表征了脱氯地杆菌在将TCE转化为顺式二氯乙烯的KB-1™亚培养物中的运动性。使用琼脂糖插塞桥方法未发现对TCE的趋化性或远离TCE的趋化性。第二个实验在无菌砂层顶部放置接种的水层,结果表明地杆菌在仅7天内就在砂层中迁移了几厘米。拟合得到地杆菌在水中的随机运动系数为0.24±0.02cm²·天⁻¹。第三个实验使用扩散池装置,其中有一个5.5厘米厚的中央砂层将DNAPL与顶部水层隔开,作为模型源区,以研究随机运动对TCE DNAPL溶解的影响。通过顶部接种,地杆菌迅速在砂层中定殖,从而提高了初始TCE DNAPL溶解通量。19天后,DNAPL溶解增强仅比砂层均匀接种低24%。建立了一个扩散-运动模型来描述扩散池中的脱氯和迁移。该模型表明,地杆菌对砂层的快速定殖是随机运动和在TCE上生长相结合的结果。

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