Interactions between laponite and microbial biofilms in porous media: implications for colloid transport and biofilm stability

• Published in: Water research (Oxford) 2004-09, Vol.38 (16), p.3614-3626
• Main Authors: Leon-Morales, C.Felipe, Leis, Andrew P., Strathmann, Martin, Flemming, Hans-Curt
• Format: Article
• Language: English
• Subjects: Applied sciences; Biofilms; Biological and physicochemical properties of pollutants. Interaction in the soil; Clay; Colloid; Colloids; Contaminant transport; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Groundwaters; Laponite; Natural water pollution; Particle Size; Pollution; Pollution, environment geology; Porosity; Porous media; Pseudomonas aeruginosa; Pseudomonas aeruginosa - growth & development; Quartz; Silicon Dioxide; Soil and sediments pollution; Soil Microbiology; Subsurface; Water Movements; Water treatment and pollution
• ISSN: 0043-1354; 1879-2448
• DOI: 10.1016/j.watres.2004.05.009

Quartz sand columns and sand-filled microscope flow cells were used to investigate the transport characteristics of the clay colloid laponite, and a biofilm-forming bacterium, Pseudomonas aeruginosa SG81. Separate experiments were performed with each particle to determine their individual transport characteristics in clean sand columns. In a second set of experiments, bacterial biofilms were formed prior to introduction of the clay colloids. In the independent transport experiments, bacteria and laponite each conformed to known physicochemical principles. A sodium chloride concentration of 7×10−2 M caused complete retention of the laponite within the sand columns. P. aeruginosa SG81 was generally less influenced by ionic strength effects; it showed relatively low mobility at all ionic strengths tested and some (albeit reduced) mobility when introduced to the columns in 1M NaCl, the highest concentration tested, but nevertheless showed reproducible trends. Under conditions favourable to laponite retention and biofilm stability (7×10−2 MNaCl), laponite suspensions were able to remobilise a portion of the attached bacterial biomass. At low ionic strength, the profile of laponite elution was also altered in the presence of a P. aeruginosa biofilm. These observations suggest that while a reduction in ionic strength has a dominant influence on the mobilisation of biological and inorganic colloids, the presence of laponite and biomass can have a distinct influence on the mobility of both types of colloids. Since these events are likely to occur in subsurface environments, our results suggest that colloid–biofilm interactions will have implications for colloid–bound contaminant transport and the remobilisation of pathogens.