INFLUENCE OF BIOFILM ACCUMULATION ON POROUS-MEDIA HYDRODYNAMICS

被引:263
作者
CUNNINGHAM, AB
CHARACKLIS, WG
ABEDEEN, F
CRAWFORD, D
机构
[1] Center for Interfacial Microbial Process Engineering, Montana State University, Bozeman
关键词
BEREA SANDSTONE; STEADY-STATE; MICROSCOPY; MODEL; CORES;
D O I
10.1021/es00019a013
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Laboratory-scale porous media biofilm reactors were used to evaluate the effect of biofilm accumulation, measured as the average thickness along a 50-mm flow path, on media porosity, permeability, and friction factor. Media tested consisted of 1-mm glass spheres, 0.70-mm sand, 0.54-mm sand, and 0.12-mm glass and sand. Pseudomonas aeruginosa was used as inoculum and 25 mg L-1 glucose substrate was continuously supplied to the reactor. Reactors were operated under constant piezometric head conditions resulting in a flow rate decrease as biofilm developed. The progression of biofilm thickness followed a sigmoidal-shaped curve reaching a maximum thickness after approximately 5 days. Media porosity decreased between 50 and 96% with increased biofilm accumulation while permeability decreased between 92 and 98%. Porous media friction factor increased substantially for all media tested. Observations of permeability in the biofilm-media matrix indicate that a minimum permeability [(3-7) X 10(-8) cm2] persisted after biofilm thickness has reached a maximum value. Such results indicate substantial interaction between mass transport, hydrodynamics, and biofilm accumulation at the fluid-biofilm interface in porous media. Improved understanding of these interactions will lead to industrial and environmental applications in biohydrometallurgy, enhanced oil recovery, and bioremediation of contaminated groundwater and soil.
引用
收藏
页码:1305 / 1311
页数:7
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