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MONOTONIC GROWTH OF MOTILE MICROORGANISMS

机译:运动微生物的单调生长

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The research results presented here are part of a more extensive effort regarding sustained bioconvection in porous media. Bio-convection is the phenomenon of gravity driven fluid motion due to buoyancy forces resulting from density differences between the fluid and motile micro-organisms suspended in the fluid. While the field of bio-convection in pure fluids emerged substantially over the past decade the corresponding effects of bio-convection in porous media received much less attention, despite the fact that micro-organisms grow naturally in porous environments; soil, food and human tissues serve as basic examples. The research focuses in two major new directions. The first deals with the theoretical and experimental investigation of bio-convection in porous media. The second major new direction is linked to the sustainability of the bioconvection motion. The existing work on bio-convection in both pure fluids and porous media exclude micro-organism growth during the bio-convection because the time scales concerned were very short. However, when the question of the sustainability of this convection over long times arises, microorganism growth has to be accounted for. If sustained bioconvection in porous media is possible it opens the avenue to investigate its impact on microbial proliferation in soil, food and human tissue, an important avenue for application of the theoretical results. Then, if bio-convection enhances microbial proliferation it may be undesirable in some cases, e.g. in food, or it might be desirable if specific micro-organisms that can be used for contaminated soil remediation will be "helped" by the bio-convection process to access contaminated regions in the soil. The theoretical and experimental results presented in this paper reflect the process of monotonic growth of motile microorganisms (e.g. the PAOI strain of Pseudomonas Aeruginosa) to be included in the bioconvection process. A new proposed model is shown to be the appropriate one to better reflect both conceptually as well as practically the microbial growth process.
机译:这里提出的研究结果是多孔介质中持续生物缺陷的更广泛努力的一部分。生物对流是引起的重力驱动流体运动的现象,由于悬浮在流体中的流体和运动微生物之间的密度差异导致的浮力力。虽然纯液中的生物对流领域在过去十年中出现了大量生物对流在多孔介质中的相应效果,但由于微生物在多孔环境中自然生长,因此较少的关注受到重视的程度较少;土壤,食品和人体组织作为基本实例。该研究重点介绍两个主要的新方向。第一批关于多孔介质生物对流的理论和实验研究。第二重要的新方向与生物检测运动的可持续性相关联。在纯净流体和多孔介质中对生物对流的现有工作排除了生物对流期间的微生物生长,因为有关时间尺度非常短。但是,当出现长时间的这种对流的可持续性问题时,必须考虑微生物增长。如果可能的多孔介质中的持续生物缺陷是可能的,它打开途径,以研究其对土壤,食物和人类组织中的微生物增殖,这是应用理论结果的重要途径的影响。然后,如果生物对流增强微生物增殖,在某些情况下可能是不希望的,例如,例如,如果在食物中,如果可用于污染的土壤修复的特异性微生物将被生物对流过程中的特异性微生物,以获得土壤中的受污染区域,则可能是可取的。本文提出的理论和实验结果反映了运动微生物的单调生长的过程(例如,铜绿假单胞菌的Paoi菌株)被包括在生物卷型过程中。新的提出模型被认为是适当的模型,以更好地在概念上反射两者以及实际上的微生物生长过程。

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