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In situ growth and activity and modes of penetration of Escherichia coli in unconsolidated porous materials.

机译:大肠杆菌在非固结多孔材料中的原位生长活性和渗透方式。

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摘要

Statistically reliable data on the in situ rates of growth, substrate consumption, and product formation are required to test the validity of the mathematical models developed for microbially enhanced oil recovery and in situ bioremediation processes. A simple, replicable porous-core system that could be aseptically divided into sections at various times was developed to follow the kinetics of microbial growth and metabolism in situ. This core system was used to study the kinetics of growth and the mode of penetration of strains of Escherichia coli through anaerobic, nutrient-saturated, fine Ottawa sand (permeability of 7.0 microns2 and porosity of 37%) under static conditions. The in situ rate of growth of a wild-type, motile, chemotactic strain, RW262, was two times slower inside cores than it was in liquid cultures. The mode of metabolism of galactose by strain RW262 was not altered inside cores, as acetate was the only product detected either inside the cores or in liquid cultures. Without applied advective force, strain RW262 grew exponentially and moved through cores at a rate of about 0.1 m/day. The cell population moved through cores in a band-like fashion, as the front of the moving cells consisted of high cell concentrations (greater than 10(5) cells per ml). Until the breakthrough of the cells occurred, galactose consumption and acetate production were observed only in the proximal sections of the core, showing that the cell propagation preceded the complete depletion of the substrate or the accumulation of large amounts of products.(ABSTRACT TRUNCATED AT 250 WORDS)
机译:需要关于原位生长速率,底物消耗和产品形成的统计可靠数据,以测试为微生物提高采油量和原位生物修复过程而开发的数学模型的有效性。开发了一个简单的,可复制的多孔核系统,该系统可以在不同的时间被无菌地分为多个部分,以追踪微生物原位生长和代谢的动力学。该核心系统用于研究大肠杆菌在静态条件下通过厌氧,营养饱和的细渥太华砂(渗透性7.0微米2和孔隙度37%)的生长动力学和菌株的渗透方式。野生型,运动型,趋化性菌株RW262的原位生长速度比液体培养慢了两倍。 RW262菌株半乳糖的代谢方式在核心内部没有改变,因为乙酸盐是核心内部或液体培养物中唯一检测到的产物。在没有施加对流力的情况下,RW262应变呈指数增长,并以约0.1 m / d的速度穿过岩心。由于移动的细胞的前部由高浓度的细胞组成(每毫升大于10(5)个细胞),所以细胞群体以带状方式穿过核心。在细胞突破之前,仅在核心的近端观察到半乳糖的消耗和乙酸盐的产生,这表明细胞增殖是在底物完全耗尽或大量产物积聚之前进行的。(摘要摘录于250话)

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