Mesoscale and microscale observations of biological growth in a silicon pore imaging element

被引:41
作者
Dupin, HJ [1 ]
McCarty, PL [1 ]
机构
[1] Stanford Univ, Dept Civil & Environm Engn, Stanford, CA 94305 USA
关键词
D O I
10.1021/es981146p
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Better physical understanding is needed of the processes affecting biological growth in aquifers, filtration beds, and recharge basins. Toward this end, a two-dimensional random width network pore model etched in a silicon wafer was developed to simulate microbial growth in porous media representative of fine sand. This Silicon Pore Imaging Element (SPIE) was seeded with a mixed culture and fed with 0.34 mM acetate under aerobic conditions and at fixed flow rate. Twelve filamentous colonies grew in a dense manner in the upgradient and lateral directions and at low density in the downgradient direction. Heterogeneous colonization led to empty zones. Particle tracking suggested rerouting of flow due to biomass growth. Microscale time-lapse measured filamentous growth rates (0.5 to 1.6 mu m/min) were in good agreement with measured mesoscale colony expansion rates. Rather than the microscale concept of biomass developing at the surface of soil grains, filamentous growth may be better represented as mesoscale colonies spanning over several pores and separated from each other by open flow channels. Biological clogging might he prevented if such flow channels could be kept open in some manner.
引用
收藏
页码:1230 / 1236
页数:7
相关论文
共 26 条
[1]   Percolation theory and network modeling applications in soil physics [J].
Berkowitz, B ;
Ewing, RP .
SURVEYS IN GEOPHYSICS, 1998, 19 (01) :23-72
[2]   Relationship between concentration and hydrodynamic boundary layers over biofilms [J].
Bishop, PL ;
Gibbs, JT ;
Cunningham, BE .
ENVIRONMENTAL TECHNOLOGY, 1997, 18 (04) :375-385
[3]   INFLUENCE OF BIOFILM ACCUMULATION ON POROUS-MEDIA HYDRODYNAMICS [J].
CUNNINGHAM, AB ;
CHARACKLIS, WG ;
ABEDEEN, F ;
CRAWFORD, D .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1991, 25 (07) :1305-1311
[4]  
Cunningham AB, 1995, WATER SCI TECHNOL, V32, P107, DOI 10.1016/0273-1223(96)00014-5
[5]   Macrotransport of a biologically reacting solute through porous media [J].
Dykaar, BB ;
Kitanidis, PK .
WATER RESOURCES RESEARCH, 1996, 32 (02) :307-320
[6]  
EHRLICH GG, 1980, 751E US GEOL SURV
[7]   Micromodel observation of the role of oil layers in three-phase flow [J].
Keller, AA ;
Blunt, MJ ;
Roberts, PV .
TRANSPORT IN POROUS MEDIA, 1997, 26 (03) :277-297
[8]   EFFECT OF LAMINAR-FLOW VELOCITY ON THE KINETICS OF SURFACE RECOLONIZATION BY MOT+ AND MOT- PSEUDOMONAS-FLUORESCENS [J].
KORBER, DR ;
LAWRENCE, JR ;
SUTTON, B ;
CALDWELL, DE .
MICROBIAL ECOLOGY, 1989, 18 (01) :1-19
[9]  
LAROCHEJAFFRENN.C, 1997, P 9 EUR S IMPR REC T
[10]   NMR IMAGING OF HYDRODYNAMICS NEAR MICROBIALLY COLONIZED SURFACES [J].
LEWANDOWSKI, Z ;
ALTOBELLI, SA ;
MAJORS, PD ;
FUKUSHIMA, E .
WATER SCIENCE AND TECHNOLOGY, 1992, 26 (3-4) :577-584