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大肠杆菌在松散多孔材料中的原位生长、活性及渗透模式

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

作者信息

Sharma P K, McInerney M J, Knapp R M

机构信息

Department of Botany and Microbiology, University of Oklahoma, Norman 73019-0245.

出版信息

Appl Environ Microbiol. 1993 Nov;59(11):3686-94. doi: 10.1128/aem.59.11.3686-3694.1993.

Abstract

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)

摘要

为了验证针对微生物强化采油和原位生物修复过程所开发的数学模型的有效性,需要有关原位生长速率、底物消耗速率和产物形成速率的统计学可靠数据。开发了一种简单、可重复的多孔岩心系统,该系统可在不同时间无菌地分割成多个部分,以跟踪原位微生物生长和代谢的动力学。该岩心系统用于研究在静态条件下,大肠杆菌菌株在厌氧、营养饱和的渥太华细砂(渗透率为7.0平方微米,孔隙率为37%)中的生长动力学和穿透模式。野生型、有运动能力、具有趋化性的RW262菌株在岩心内部的原位生长速率比在液体培养物中慢两倍。RW262菌株在岩心内部对半乳糖的代谢模式没有改变,因为无论是在岩心内部还是在液体培养物中,检测到的唯一产物都是乙酸盐。在没有施加平流力的情况下,RW262菌株呈指数生长,并以约0.1米/天的速度穿过岩心。细胞群体以带状方式穿过岩心,因为移动细胞的前沿由高细胞浓度(每毫升大于10(5)个细胞)组成。在细胞突破之前,仅在岩心的近端部分观察到半乳糖消耗和乙酸盐产生,这表明细胞繁殖先于底物的完全耗尽或大量产物的积累。(摘要截短于250字)

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本文引用的文献

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Appl Environ Microbiol. 1985 Aug;50(2):383-91. doi: 10.1128/aem.50.2.383-391.1985.
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Appl Environ Microbiol. 1989 Sep;55(9):2280-6. doi: 10.1128/aem.55.9.2280-2286.1989.

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