Dynamics of biomass membrane filtration

ENVR 89

Slawomir W. Hermanowicz, hermanowicz@ce.berkeley.edu1, J. W. Cho2, R. Shane Trussell3, Rion P. Merlo4, and David Jenkins1. (1) Department of Civil and Environmental Engineering, University of California, 629 Davis Hall, Berkeley, CA 94720-1710, (2) Korea Institute of Science and Technology, Seoul, 130-650, South Korea, (3) Trussell Technologies, Inc, 232 N. Lake Ave., Ste. 300, Pasadena, CA 91101, (4) Brown and Caldwell, 201 N. Civic Dr., Ste. 115, Walnut Creek, CA 94596
Common framework describes membrane filtration as a combination of forward flux with filtered fluid and mechanisms moving the solids away from the membrane surface (backflux). We extend this model to dynamic conditions by assuming that a solid's network is formed adjacent to the membrane surface. The critical solid's concentration is theoretically derived from the percolation theory. The hydrodynamic stress leads to further network deformation and to a decrease in porosity and permeability. At some moment, the porosity of the solid's network becomes so small that the pores (voids) become disconnected and an impermeable cake is formed. Based on theoretical considerations, the loss of connectivity should be very rapid, reminiscent of a phase transition. Our model successfully describes such dramatic changes during “subcritical” fouling. Finally, the model is able to explain the effects of the time dependence of filtration resistance responses to biomass changes as observed in our experiments with dead-end filtration.