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Published on: December 24, 2014
Bacterial transport experiments in fractured crystalline bedrock
Matthew W Becker1, David W Metge, Samantha A Collins
1Department of Geology, University at Buffalo, Buffalo, NY 14260, USA. mwbecker@geology.buffalo.edu
Bacterial transport in groundwater bedrock is crucial for contaminant biodegradation. Minor physical differences in bacteria significantly impact their movement and distribution at the field scale.
Area of Science:
- Environmental Microbiology
- Hydrogeology
- Biogeochemistry
Background:
- Groundwater contaminant biodegradation relies on the transport of degrading bacteria.
- Limited data exist on bacterial transport in saturated bedrock at the field scale.
Purpose of the Study:
- To investigate the transport behavior of different bacterial strains in fractured crystalline bedrock.
- To compare bacterial transport with microsphere tracers under field conditions.
Main Methods:
- Conducted forced-gradient tracer experiments over 36 meters in fractured bedrock.
- Utilized differentially stained bacteria with varying physicochemical and physiological properties (shape, cell-wall type, motility).
- Compared bacterial transport to that of microsphere tracers.
Main Results:
- No two bacterial strains exhibited identical transport behavior.
- Microspheres showed distinct breakthrough curves compared to bacteria.
- Nonmotile bacteria showed better recovery than motile strains.
- Gram-negative rods had higher recovery than Gram-positive rods of similar size.
- Spherical bacteria generally transported better than rod-shaped bacteria.
Conclusions:
- Bacterial physical properties, such as motility and cell shape, significantly influence transport in saturated bedrock.
- Even minor differences in bacterial characteristics can lead to substantial variations in field-scale transport.
- Findings are specific to the studied bacterial strains and groundwater environment but suggest broader implications for microbial transport modeling.
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