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The initial adhesion of micro‐organisms on solid surfaces strongly affects their transport and fate in soil and aquatic environments. Experiments on Bacillus subtilis with various soil minerals (including kaolinite, montmorillonite, goethite, birnessite, quartz and mica) were conducted to determine the role of surface properties in adhesion and to test the validity of the extended Derjaguin, Landau, Verwey and Overbeek (DLVO) theory for bacterial adhesion. Adhesion of B. subtilis on all six minerals conformed to the Langmuir equation. Adhesion capacity and affinity showed a significant correlation with the specific external surface area (SESA) of the minerals and the calculated electrostatic energy barrier, respectively, but no significant correlation was observed between hydrophobicity and the adhesion parameters. These results demonstrate that adhesion capacity and affinity are primarily controlled by the SESA of the minerals and the surface electrical properties, respectively. The dependence of the adhesion capacity on SESA may be explained by the cell–mineral interaction model. Adhesion could be well predicted by the extended DLVO theory. The initial adhesion of bacteria with soil minerals can be evaluated by using independently measured surface properties of these components based on the extended DLVO theory combined with the Langmuir equation.

Soil components (e.g., clays, bacteria and humic substances) are known to produce mineral-organic composites in natural systems. Herein, batch sorption isotherms, isothermal titration calorimetry (ITC), and Cd K-edge EXAFS spectroscopy were applied to investigate the binding characteristics of Cd on montmorillonite(Mont)-humic acid(HA)-bacteria composites. Additive sorption and non-additive Cd(II) sorption behaviour is observed for the binary Mont-bacteria and ternary Mont-HA-bacteria composite, respectively. Specifically, in the ternary composite, the coexistence of HA and bacteria inhibits Cd adsorption, suggesting a “blocking effect” between humic acid and bacterial cells. Large positive entropies (68.1 ~ 114.4 J/mol/K), and linear combination fitting of the EXAFS spectra for Cd adsorbed onto Mont-bacteria and Mont-HA-bacteria composites, demonstrate that Cd is mostly bound to bacterial surface functional groups by forming inner-sphere complexes. All our results together support the assertion that there is a degree of site masking in the ternary clay mineral-humic acid-bacteria composite. Because of this, in the ternary composite, Cd preferentially binds to the higher affinity components-i.e., the bacteria.

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