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MONOTONIC GROWTH OF MOTILE MICROORGANISMS

机译:分子微生物的单调生长

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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:此处提出的研究结果是有关多孔介质中持续生物对流的一项更广泛工作的一部分。生物对流是由于流体与悬浮在流体中的微生物之间的密度差而产生的浮力引起的重力驱动的流体运动现象。尽管在过去的十年中,纯流体中的生物对流领域大为兴起,但尽管微生物在多孔环境中自然生长,但在多孔介质中生物对流的相应影响却很少受到关注。土壤,食物和人体组织就是基本例子。该研究集中在两个主要的新方向。第一部分涉及多孔介质中生物对流的理论和实验研究。第二个主要的新方向与生物对流运动的可持续性有关。现有的在纯流体和多孔介质中生物对流的研究都排除了生物对流过程中微生物的生长,因为相关的时间尺度非常短。但是,当出现长时间对流可持续性的问题时,就必须考虑微生物的生长。如果可以在多孔介质中进行持续的生物对流,则将为研究其对土壤,食物和人体组织中微生物繁殖的影响开辟道路,这是应用理论结果的重要途径。然后,如果生物对流促进微生物增殖,则在某些情况下可能是不希望的,例如食物中的微生物,或者如果希望通过生物对流过程“帮助”进入土壤污染区域的微生物“修复”可用于污染土壤修复的特定微生物,则可能是理想的。本文提出的理论和实验结果反映了将要包括在生物对流过程中的运动型微生物(例如铜绿假单胞菌的PAOI菌株)的单调生长过程。新提出的模型被证明是合适的模型,可以更好地在概念上和实践上反映微生物的生长过程。

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