2008
DOI: 10.1128/aem.00313-08
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The Porous Surface Model, a Novel Experimental System for Online Quantitative Observation of Microbial Processes under Unsaturated Conditions

Abstract: Water is arguably the most important constituent of microbial microhabitats due to its control of physical and physiological processes critical to microbial activity. In natural environments, bacteria often live on unsaturated surfaces, in thin (micrometric) liquid films. Nevertheless, no experimental systems are available that allow real-time observation of bacterial processes in liquid films of controlled thickness. We propose a novel, inexpensive, easily operated experimental platform, termed the porous sur… Show more

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Cited by 54 publications
(90 citation statements)
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“…The mild matric potential that we prescribed does not per se restrict bacterial motion (12), but it acts through its control of the effective liquid-film thickness on the ceramic-plate surface. The relationship between matric potential and liquid-film thickness depends solely on surface wettability and roughness (15).…”
Section: Resultsmentioning
confidence: 99%
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“…The mild matric potential that we prescribed does not per se restrict bacterial motion (12), but it acts through its control of the effective liquid-film thickness on the ceramic-plate surface. The relationship between matric potential and liquid-film thickness depends solely on surface wettability and roughness (15).…”
Section: Resultsmentioning
confidence: 99%
“…The PSM allows growing and observing fluorescent cells at the surface of a porous ceramic plate (diameter = 4.2 cm; maximum pore size = 1.7 μm) under prescribed suction, which controls surface liquidfilm thickness (12). Liquid FAB medium with 5 mM benzoate as the sole carbon source was used to wet the plate and sustain microbial growth.…”
Section: Methodsmentioning
confidence: 99%
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“…Self-propulsion by rotating flagella is the common form of motion among many motile prokaryotes in aqueous environments [Grossart et al, 2001]. Other forms of motility such as swarming, gliding, twitching, and sliding are limited to a few species [Harshey, 2003;Dechesne et al, 2008]. Microbial life in natural soils under most climatic conditions is characterized by motion in small pores and in thin liquid films governed by low Reynolds numbers that also limit the role of passive (advective) transport to a few rare events where the soil becomes very wet [Purcell, 1977;Bitton and Harvey, 1992;Fenchel, 2002;Berg, 2005;Or et al, 2007].…”
Section: Introductionmentioning
confidence: 99%