1991
DOI: 10.1128/aem.57.1.190-193.1991
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Relationship between Cell Surface Properties and Transport of Bacteria through Soil

Abstract: A study was conducted to relate the properties of Enterobacter, Pseudomonas, Bacillus, Achromobacter, Flavobacterium, and Arthrobacter strains to their transport with water moving through soil. The bacteria differed markedly in their extent of transport; their hydrophobicity, as measured by adherence to n-octane and by hydrophobic-interaction chromatography; and their net surface electrostatic charge, as determined by electrostatic interaction chromatography and by measurements of the zeta potential. Transport… Show more

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Cited by 306 publications
(117 citation statements)
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“…clay-dominated geology), given the same rainfall event, a proportionally greater volume of water is likely to flow over the surrounding floodplain soil, picking up soil particles and associated microorganisms before reaching a receiving stream or river. Microbial size (Gannon, Manilal, & Alexander, 1991) and cell surface characteristics, as well as soil properties (Huysman & Verstraete, 1993) and the presence of preferential flow pathways in the soil such as macropores (Martins et al, 2013) could affect the size and composition of the transported community. In addition to geology, magnitude and duration of rainfall event, and time of year are also important; greater volumes of runoff will enter streams following high-intensity and/or long-duration storm events especially when antecedent soil moisture deficit is low (Heppell et al, 2002).…”
Section: (1) Community Coalescence In Headwatersmentioning
confidence: 99%
“…clay-dominated geology), given the same rainfall event, a proportionally greater volume of water is likely to flow over the surrounding floodplain soil, picking up soil particles and associated microorganisms before reaching a receiving stream or river. Microbial size (Gannon, Manilal, & Alexander, 1991) and cell surface characteristics, as well as soil properties (Huysman & Verstraete, 1993) and the presence of preferential flow pathways in the soil such as macropores (Martins et al, 2013) could affect the size and composition of the transported community. In addition to geology, magnitude and duration of rainfall event, and time of year are also important; greater volumes of runoff will enter streams following high-intensity and/or long-duration storm events especially when antecedent soil moisture deficit is low (Heppell et al, 2002).…”
Section: (1) Community Coalescence In Headwatersmentioning
confidence: 99%
“…The physicochemical properties of the cell surfaces are known to control the interactions between microorganisms and interfaces. The assessment of microbial cell surface hydrophobicity as one of the surface properties influencing microbial adhesion and transport in heterogeneous media has been well established (van Loosdrecht et al ., 1987;Gannon et al ., 1991). Methods such as microbial adhesion to hydrocarbons (MATH), hydrophobic interaction chromatography (HIC) and contact angle measurements (CAM) are widely used (reviewed in Doyle and Rosenberg, 1990).…”
Section: Introductionmentioning
confidence: 99%
“…to soil, that adsorption was greater to a clay loam than to a sandy soil, and that adsorption could be increased in the presence of divalent cations. Gannon et al [28] noted that even when bacterial cells were grown under identical conditions, the nonuniformity of the bacterial surface may cause a bacterium to be hydrophilic in one assay and hydrophobic in another. Clearly, many physicochemical and microbiological factors influence the adsorption of bacteria to soil, and Lawrence and Hendry [29] have reviewed these in more detail.…”
Section: Discussionmentioning
confidence: 99%