TY - JOUR
T1 - Biofilm development and the dynamics of preferential flow paths in porous media
AU - Bottero, Simona
AU - Storck, Tomas
AU - Heimovaara, Timo J.
AU - van Loosdrecht, Mark C.M.
AU - Enzien, Michael V.
AU - Picioreanu, Cristian
N1 - Generated from Scopus record by KAUST IRTS on 2022-09-13
PY - 2013/10/1
Y1 - 2013/10/1
N2 - A two-dimensional pore-scale numerical model was developed to evaluate the dynamics of preferential flow paths in porous media caused by bioclogging. The liquid flow and solute transport through the pore network were coupled with a biofilm model including biomass attachment, growth, decay, lysis, and detachment. Blocking of all but one flow path was obtained under constant liquid inlet flow rate and biomass detachment caused by shear forces only. The stable flow path formed when biofilm detachment balances growth, even with biomass weakened by decay. However, shear forces combined with biomass lysis upon starvation could produce an intermittently shifting location of flow channels. Dynamic flow pathways may also occur when combined liquid shear and pressure forces act on the biofilm. In spite of repeated clogging and unclogging of interconnected pore spaces, the average permeability reached a quasi-constant value. Oscillations in the medium permeability were more pronounced for weaker biofilms. © 2013 Taylor & Francis.
AB - A two-dimensional pore-scale numerical model was developed to evaluate the dynamics of preferential flow paths in porous media caused by bioclogging. The liquid flow and solute transport through the pore network were coupled with a biofilm model including biomass attachment, growth, decay, lysis, and detachment. Blocking of all but one flow path was obtained under constant liquid inlet flow rate and biomass detachment caused by shear forces only. The stable flow path formed when biofilm detachment balances growth, even with biomass weakened by decay. However, shear forces combined with biomass lysis upon starvation could produce an intermittently shifting location of flow channels. Dynamic flow pathways may also occur when combined liquid shear and pressure forces act on the biofilm. In spite of repeated clogging and unclogging of interconnected pore spaces, the average permeability reached a quasi-constant value. Oscillations in the medium permeability were more pronounced for weaker biofilms. © 2013 Taylor & Francis.
UR - http://www.tandfonline.com/doi/abs/10.1080/08927014.2013.828284
UR - http://www.scopus.com/inward/record.url?scp=84888004661&partnerID=8YFLogxK
U2 - 10.1080/08927014.2013.828284
DO - 10.1080/08927014.2013.828284
M3 - Article
SN - 0892-7014
VL - 29
SP - 1069
EP - 1086
JO - Biofouling
JF - Biofouling
IS - 9
ER -