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MODELING SUBSURFACE PROCESSES
This article also appears in the Oak Ridge National Laboratory
Review (Vol. 26, No. 1), a quarterly research and development
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Recently I spent a day in California looking at hydraulic fluid
spills beneath old garages for servicing motor vehicles. Apparently
hydraulic lifts leak small amounts of fluid. As a result, plumes of
hydraulic fluid percolate through the ground and eventually may
contaminate groundwater. At some time these sites must be cleaned
up. However, to accomplish this task we must know where the
contaminant is and where it will move as a result of cleanup
activities. As with other subsurface problems, this question
arises: Can soil samples at the contamination site provide an
accurate picture of the location of specific contaminants?
Unlike our more traditional areas of engineering, knowledge of
subsurface flows is made difficult by the enormous uncertainty of
the data collected. For example, a hapless engineer may insert a
chemical-sensing probe at the very spot where a weary traveler
spilled some unwanted soda pop the night before. In this case, the
environment created for the sensor may be totally different from
that of the rest of the site. This uncertainty is made more
critical by the large cost of collecting soil data--possibly
reaching several thousand dollars for a single sampling point.
Thus, it is critical that methods be developed soon for economical
sampling of possibly contaminated sites.
Statisticians have developed sampling methods that seem almost
miraculous. For example, within a few minutes after polls have
closed, statistical methodology makes surprisingly precise election
predictions. Their methodology is based on so-called "probability"
models in which the parameters of interest are permitted to be
random but are dictated by certain "probability distributions"
indicating that random parameters are inclined to be nearer to
certain values than others--much the same as heights of people or
the way people vote in elections.
These distributions have been found on the basis of exhaustive
analysis of past elections and the determination of small but
highly representative subsamples of the population. Peculiarities
of certain subcollections of parameters (e.g., teenagers enjoying
louder noises than do their parents) are taken into account for the
sampling process. For subsurface processes, sources of such special
behavior might include soil strata, hills, and the history of the
site of interest.
For many years mathematicians and engineers have developed
deterministic (nonprobabilistic) models of flow in soil. These
models, however, require precise knowledge of such features as
contaminant distributions at some initial time and soil parameters
at depth. Hence, they are not wholly suitable for the "real world"
problem in which such knowledge is not really available.
Recently, statisticians and mathematicians at ORNL have broken new
ground by melding their respective perceptions of subsurface
events. The mathematicians have models that are totally
deterministic, whereas the statisticians have models that are
wholly geared to data. By joining forces they have produced new
tools that promise substantially improved sampling methods. They
will be able to better answer questions of when and where to take
samples and what kinds. Their approach is to "teach" the
probability distributions to reflect the underlying behavior of
processes when they are used to guide the sampling process. The
teaching process uses a combination of tools drawn from partial
differential equations on one hand and sampling theory on the
other.
Using these and similar approaches, eventually an environmental
engineer can go to a site needing cleanup and determine from a
dialogue with a computer where and when to sample the site to get
the most nearly accurate view of underground contamination. Such a
capability may even allow the engineer to say with certainty,
"Someone spilled some soda here last night."
Alan D. Solomon
(keywords: sampling, environmental modeling)
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Date Posted: 1/26/94 (ktb)