Adhesion of bacteria onto solid surfaces is a necessary event in nature for
the utilization of inorganic and organic values and for the enhanced growt
h of bacteria. Interactions between Paenibacillus polymyxa, with different
minerals such as hematite, corundum and quartz are examined in this work in
the light of Derjaguin, Landau, Verwey and Overbeek theory, popularly know
n as DLVO theory and possible chemical interactions. The adhesion process i
s normally controlled initially by physicochemical interactions between cel
ls and mineral substrates and subsequently by the production of extra cellu
lar polymers to make the attachment stronger, From this study, it is clear
that maximum adsorption of cells on hematite and corundum occurs at a pH be
low the isoelectric point, whereas in the case of quartz the adsorption of
cells remained almost constant in the entire pH range studied. From adhesio
n tests, it is also clear that the above bacteria adsorb preferentially on
hematite and corundum than on quartz. It is obvious from the interaction en
ergy calculations that the columbic forces play a major role in the interac
tion of P. polymyxa with hematite, corundum and quartz. Although the columb
ic forces do play such a role, it is evident from the Fourier Transform Inf
rared Spectroscopy (FTIR) results that other forces such as chemical forces
are also involved simultaneously. (C) 2001 Published by Elsevier Science B
.V.