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Subsections
5.4 Case Study IV: A Ground Water Model with Discontinuous Probability
Distributions
Characterization of exposure due to leakage of hazardous contaminants from a
land disposal unit involves significant uncertainty due to inherent
variability in the hydrogeologic properties of the site, and due to
incomplete understanding of the processes involved in transport of
contaminants. Since the exposure estimates are utilized in making policy
decisions, it is important that any exposure characterization should take
into account the variability and uncertainty involved with the physical
system, and with the modeling process.
Here, a case study is presented in relation to characterization of
uncertainty in estimated tritium exposure at a receptor well. The main
source for the contamination is a hypothetical landfill unit in the southern
United States. The fate and transport model used in this work is the EPA's
Composite Model for leachate Migration and Transformation Products
(EPACMTP). In the following sections, a brief description of the model used,
the estimates of the model parameters and the uncertainty analysis methods
is given. The variability and uncertainty associated with the hydrogeologic
parameters and with the physical properties of the landfill unit are
considered to characterize the uncertainty in the calculated concentrations
of tritium. Environmental metrics considered are the estimated maximum
concentration of tritium in a ``receptor'' well and the estimated time of
occurrence of the maximum concentration.
The EPA's Composite Model for leachate Migration and Transformation Products
(EPACMTP) provides estimates of potential human exposure to hazardous
chemicals leaching from land disposal facilities [64].
EPACMTP simulates the subsurface fate and transport of contaminants released
from land disposal sites, and predicts the associated groundwater exposure
in a domestic drinking water receptor well. This model is an improvement
over the EPA's Composite Model for Landfills (EPACML) [62]. EPACML
accounts for the first-order decay and sorption of chemicals, but disregards
the formation and transport of transformation products. In addition, EPACML
can describe only uniform, unidirectional groundwater flow. On the other
hand, EPACMTP can take into consideration: (i) chain decay reactions and
transport of daughter and grand-daughter products, (ii) effects of
water-table mounding on groundwater flow and contaminant migration, (iii)
finite source as well as continuous source scenarios, and (iv) metals
transport.
EPACMTP consists of two modules: an unsaturated zone module called Finite
Element and semi-analytical Contaminant Transport in the Unsaturated
Zone (FECTUZ), and a saturated zone module called Combined
Analytical-Numerical SAturated Zone in 3-Dimensions (CANSAZ-3D). FECTUZ is a
one-dimensional model that simulates vertically downward steady-state flow
and contaminant transport through the unsaturated zone above an unconfined
aquifer. CANSAZ-3D simulates 3-D steady-state groundwater flow and transient
or steady state contaminant transport. EPACMTP currently uses a simplified
2-D version of the CANSAZ-3D, and the modules are optimized for
computational efficiency. Appendix D provides detailed
description of the formulation and implementation of FECTUZ and CANSAZ-3D
modules.
Data for the site characteristics, infiltration rates, the volume and
area of the landfills, and the probability distributions for the
hydrogeologic parameters are obtained from a review conducted by the
Hydrogeologic Inc. [64]. In this review, a number of
different sources were used for the development of this site-based
approach. Four of these sets were selected to derive the regional
characteristics of important parameters for each sampled site:
- the OPPI survey of waste management units (EPA,1986),
- the infiltration and recharge analysis performed by OSW,
- the USGS state-by-state inventory of groundwater resources, and
- the Hydrogeologic Database for Modeling (HGDB), developed from a
survey of hazardous waste field sites in the U.S.
These datasets were used in conjunction with the soil mapping database
provided by the Soil Conservation Service (SCS), the data sets from the
National Oceanic and Atmospheric Administration, and simulations from the
HELP model [180]. The data for the hypothetical scenario in
this case study were adapted from a data set provided by Hydrogeologic
Inc.
The Monte Carlo method requires that for each input parameter that has
associated uncertainty or variability, a probability distribution (or
a frequency distribution) be provided. The method involves the
repeated generation of pseudo-random values of the uncertain input
variables (drawn from the known distribution and within the range of
any imposed bounds) and the application of the model using these
values to generate a set of model responses or outputs (for example,
the receptor well concentration,
). These responses are then
statistically analyzed to yield the probability distribution of the
model output. The various steps involved in the application of a Monte
Carlo simulation are:
- selection of representative cumulative probability distribution
functions for the relevant input variables,
- generation of a pseudo-random number from the selected
distributions, representing a possible set of values (a realization)
for the input variables,
- checking whether the realization satisfies the constraints or
bounds on the distribution (and resampling till a reasonable
realization is obtained),
- application of the model to compute the derived inputs and
outputs,
- repeated application of the above steps for a specified number
of iterations, and
- statistical analysis of the series of the output values generated.
Table 5.3:
Probability
distributions used for the EPACMTP model
parameters for the uncertainty analysis
 |
This case study consists of a site based landfill modeling for tritium
contamination at a groundwater well resulting from a hypothetical landfill
unit in the souther United States. The landfill is a finite source, of
0.35 km
area, with a leaching duration of 20 years, and a recharge rate
of 0.381 m/yr. The receptor well is located at a distance of 1635 m from
the landfill. The EPACMTP model is used to simulate the radioactive decay
and transport of tritium through the saturated and unsaturated zone
underlying the landfill. The data used here is adapted from data provided by
Hydrogeologic Inc.
The probability distributions of the site-specific parameters for the
land fill at the Old Burial Ground are given in
Table 5.3, and the values of the constant model
parameters for EPACMTP are given in Table 5.4.
Table 5.4:
Deterministic
Parameters in the EPACMTP model
for the case study
 |
Figure 5.21 shows the uncertainty associated with the
estimation of maximum tritium concentration in the ground water, as a
result of the leaching from the landfill unit. Figure 5.22
shows the uncertainty associated with the estimated time
of occurrence of the maximum tritium concentration in the ground water at
the well. The figures show the pdfs estimated by the Monte Carlo
simulations and by the SRSM. Results of the SRSM with 350 model runs are
compared with those of Monte Carlo simulations with 1000, 3000 and 5000
model runs.
Figure 5.21:
Uncertainty in estimated maximum tritium concentration in a
receptor well
 |
Figure 5.22:
Uncertainty in estimated time of occurrence of maximum
tritium concentration in a receptor well
 |
The results indicate that the SRSM shows close agreement with the Monte
Carlo results, while requiring much fewer number of runs. Further, there are
certain other advantages in using the SRSM, that are focused in the ongoing
research:
- The relationships between inputs and outputs can be
easily estimated, since both the input and output pdfs are expressed as
a series expansion in srvs. This implies that SRSM provides insight into
the relative contribution of each uncertain input each output, thus giving
extensive sensitivity and uncertainty information. Conventional Monte
Carlo methods do not provide such information.
- Correlation between outputs can be easily estimated since all
outputs are expressed in terms of srvs. On the other hand, Monte Carlo
methods require significantly large number of model simulations to obtain
a reasonably good approximation of the correlation between outputs.
- The algebraic expressions for the outputs in terms of the srvs are
smooth and continuous and could efficiently model the tails of the
probability distributions of the outputs (which typically correspond to
either high risk or worst case scenarios).
One of the limitations of the Stochastic Response Surface Method, that
is a focus of the ongoing research, is as follows: the current
implementation of the SRSM does not take into account constraints on
the input probability distributions that make the distributions
discontinuous. In short, this method assumes that the probability
distributions are continuous. In the present work, such constraints
are modeled as truncated probability distributions, and the results
shown in Figures 5.21 and 5.22 for the SRSM
are obtained in such a manner, indicating that they represent only an
approximate estimate. Current work in progress involves the refinement of
the SRSM so that all types of constraints can be propagated, and
discontinuities in probability distributions can be fully addressed.
Next: 6. CHARACTERIZATION AND REDUCTION
Up: 5. CASE STUDIES FOR
Previous: 5.3 Case Study III:
Sastry S. Isukapalli
1999-01-19