Predictions of TCE Plume Expansion Using Calibration-Constrained Monte Carlo Analysis

Monday, April 12, 2010: 1:50 p.m.
Tabor Auditorium (Westin Tabor Center, Denver)
Gregory W. Council, PE , GeoTrans (a Tetra Tech company), Roswell, GA
James L. Ross, Ph.D. , GeoTrans (a Tetra Tech company), Roswell, GA
The Tooele Army Depot (TEAD) is located approximately 35 miles southwest of Salt Lake City, Utah. Past releases at this site resulted in a TCE plume that is currently over 3 miles long. The shape and trajectory of the plume are controlled to a large extent by low-permeability fault zones.  The plume has also been influenced by a groundwater extraction/injection system that was operated from 1994 to 2004. A groundwater flow and transport model of the TEAD site was developed in 1994 and further analyses have resulted in many improvements to the model.  The model, which now uses the SEAWAT simulator, is used to assess the extent of future TCE plume migration.  The model is an important tool used in the groundwater management strategy for TEAD.

In 2008, stochastic parameter uncertainty was incorporated into the TEAD model to better address the potential range of future plume migration.  Probability distribution functions for model parameters were determined based on field data and prior studies.  Monte Carlo analysis propagated uncertainty in model parameters to predictions of TCE transport. However, few realizations of model parameter values resulted in reasonable model calibration, calling into question the range and likelihood of predictions.

In 2009, the modeling analysis utilized PEST to (a) improve model calibration and (b) constrain the Monte Carlo analysis using the calibration data.  The use of advanced features such as regularization and singular-value decomposition significantly  reduced the statistical model-to-measurement calibration error.  Regulatory priorities were addressed by adjusting observation weights in areas of potential concern.  Also, the application of null-space Monte Carlo analysis in PEST improved the uncertainty analysis by automatically transforming parameter sets to achieve calibration. The application of these methods to the TEAD model resulted in a more complete assessment of possible plume migration than was possible with previous deterministic and stochastic models.