Dynamics of reactive microbial hotspots in concentration and velocity gradients
Abstract
n subsurface environments, bacteria play a major role in controlling the kinetics of a broad range of bio-
geochemical reactions. In such environments, nutrients
uxes and solute concentrations needed for bacteria
metabolism may be highly variable in space and intermittent in time. This can lead to the formation of reactive
hotspots where and when conditions are favorable to particular microorganisms, hence inducing biogeochemical
reaction kinetics that dier signicantly from those measured in homogeneous model environments. To investi-
gate the impact of chemical gradients on the spatial structure and growth dynamics of subsurface microorganism
populations, we develop micro
uidic cells allowing for a precise control of
ow and chemical gradient conditions,
as well as quantitative monitoring of the bacteria's spatial distribution and early-stage biolm development.
Using the non-motile Escherichia coli JW1908-1 strain and Gallionella capsiferriformans ES-2 as model
organisms, we investigate the behavior and development of bacteria over a range of single and double con-
centration gradients in the concentrations of nutrients, electron donors and electron acceptors. We measure
bacterial activity and population growth locally in precisely known hydrodynamic and chemical environments.
This approach allows time-resolved monitoring of the location and intensity of reactive hotspots in micromodels
as a function of the
ow and chemical gradient conditions. We compare reactive microbial hotspot dynamics in
our micromodels to classic growth laws and well-known growth parameters for the laboratory model bacteria
Escherichia coli, namely Michaelis-Menten-Monod nutrients uptake and Doop's growth law.
The validated growth laws are then integrated into a mixing model quantifying the dynamics of nutrient
gradients in shear
ows. The main objective is to investigate the in
uence of combined chemical and velocity
gradients on biogeochemical reactions kinetics and biomass production. We discuss the consequences of these
results in the context of biomass production in heterogeneous velocity and chemical gradients.