1st
Quarter Measures
(Istok, due 12/31/05) |
Report results of
updated small-scale model using recent advances in
understanding of coupled thermodynamic and biologic
factors to predict changes in Oak Ridge Field Research
Center microbial community composition in response
to exogenous alterations in subsurface chemistry. |
1st
Quarter Results |
This report summarizes the most recent results
of the research project “Stability of U(VI)
and Tc(VII) Reducing Microbial Communities to Environmental
Perturbation: Development and Testing of a Thermodynamic
Network Model” that is attempting to
model (predict) the effect of exogenous chemical
amendments on the subsurface microbial community
at the Oak Ridge Field Research Center (FRC). The
model explicitly couples the thermodynamics of
microbial growth and geochemical reactions to make
quantitative system-specific predictions of microbial
community dynamics. Model predictions are
being tested with the results of small- to intermediate-scale
field experiments.
1. Overall Objective and Hypothesis
The overall goal of this project is to develop and test a thermodynamic
network model for predicting the effects of substrate additions and
environmental perturbations on the composition and functional stability
of subsurface microbial communities. The overall scientific hypothesis
is that a thermodynamic analysis of the energy-yielding reactions performed
by broadly defined groups of microorganisms can be used to make quantitative
and testable predictions of the change in microbial community composition
and system geochemistry (including contaminant chemistry) that occur
when a substrate is added to the subsurface or when environmental conditions
change.
2. Types of Investigations Performed
Our research consists of three main activities:
a. Model Development: A list of the major
microbial groups present in samples of groundwater
and sediment from the FRC has been compiled. Computer
programs have been developed to compute the overall
growth reaction and governing thermodynamic quantities
for each group. Necessary model input parameters
(electron transfer efficiencies) are being estimated
from large numbers of published laboratory experiments. The
output from this activity is a thermodynamic data
base containing the chemical stoichiometry and
standard state free energy change that defines
the growth of each group (e.g. denitrifiers, iron
reducers, etc.). Collectively these calculations
define the growth reactions and energy flows in
an intact microbial community.
b. Numerical Simulations: The thermodynamic
data base is combined with existing geochemical
data and used to predict equilibrium reaction paths
that show the coupled changes in microbial community
composition and system geochemistry that occur
when amendments are added to the subsurface. Simulations
are being performed to investigate the effect of
ethanol additions on uranium and technetium bioimmobilization
for the major subsurface environments at the FRC
(Areas 1 and 3 with neutral pH and low nitrate
groundwater; and Area 2 with low pH and high nitrate
groundwater). Inputs include measured chemical
quantities on sediment and groundwater; outputs
include predicted changes in groundwater and sediment
chemistry and microbial community composition. Model
predictions have been consistent with field observations
and provide important insights into the role of
specific microbial groups (esp. denitrifiers) on
overall system response. Model predictions
are being used to investigate alternate bioimmobilization
strategies (choice of substrate, sulfate additions,
etc.) and to predict the long-term stability of
bioreduced uranium and technetium to changing environmental
conditions.
c. Experimental Verification: Ultimately
model predictions must be verified by direct measurement
and we have assembled a suite of lipid and nucleic
acid-based biomarkers for this purpose. We
are developing a “dictionary” that
will allow predicted growth of defined microbial
groups to be detected and quantified by one or
more distinct biomarkers. Model predictions
for long-term experiments in small-scale microcosms
and intermediate-scale physical models and for
short-term small-scale field experiments are being
compared with biomarker data collected on groundwater
and sediment samples. Initial comparisons
are made on total biomass and groups with known
functional genes. Particular emphasis is
placed on denitrifiers, sulfate reducers, and iron
reducers as these make up the largest portion (> 90
% in some cases) of the entire community following
substrate addition. We are actively collaborating
with several NABIR investigators to apply model
simulations to other experimental systems.
3. Main Results
The most recent results of our project are summarized here:
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The predicted microbial community composition
varies greatly from one site to the next in
response to electron donor additions. Principal
factors are the concentrations of available
electron acceptors, primarily oxygen, nitrate,
sulfate, iron, and manganese.
-
Denitrification, fermentation, and sulfate-,
iron-, and manganese-reduction are the major
microbial processes in all environments tested.
-
pH has a relatively small effect on microbial
community response to donor addition. Microbial
bicarbonate production rapidly increases the
pH in initially low pH environments.
-
Low concentrations of uranium and technetium
provide very little energy to microorganisms
and microbial uranium and technetium reduction
consume only trivial amounts of added electron
donor.
-
Bioreduced uranium can be readily reoxidized
by oxidized groundwater once electron donor
additions ceases; bioreduced technetium is
more resistant to reoxidation
4. Planned Activities:
The activities planned for the coming year include:
-
We are continuing to refine the numerical
model to include additional groups of microorganisms
and additional microbial processes to better
align the model with observations from laboratory
and field experiments. In particular
we wish to include groups that are involved
in the oxidation of sulfide, ferrous iron,
and bioreduced uranium.
-
We will design a series of laboratory microcosm
experiments to explicitly test model predictions
for a range of defined conditions. In
these experiments, sufficient data will be
collected to monitor changes in geochemistry
and microbial community composition during
both bioreduction and reoxidation.
-
We will collaborate with other NABIR investigators
to test the model’s utility for interpreting
laboratory and field data and for transferring
results from one system to another.
-
A series of numerical simulations will be
conducted to quantify the stability of an
intact microbial community to various environmental
perturbations including changing pH, nitrate
concentration, and donor availability.
5. Project Significance: This project
is clearly showing that the ability to predict
the effects of donor addition on change inmicrobial
community composition is essential for creating
conditions that favor the long-term stability of
bioreduced uranium and technetium. Moreover,
the ability of a microbial community to maintain
functional stability (i.e. maintain high rates
of uranium and technetium reduction) when subjected
to various environmental perturbations is of critical
importance for the ultimate use of bioimmobilization
at DOE legacy waste sites. The longer-term
significance of this project will be to provide
a comprehensive theoretical framework for designing
and interpreting complex field experiments and
to aid in “bridging-the-gap” between
basic research and field applications. |
2nd
Quarter Measures
(Parker, due 3/31/05) |
Run updated large-scale
3-D flow and chemical transport model for the Oak
Ridge Field Research Center site based on new information
on biogeochemistry, groundwater and subsurface media. |