Abstract
This paper describes a multidisciplinary endeavor to develop and employ basic research strategies for guiding remediation efforts in contaminated fractured subsurface media at the U.S. Department of Energy’s Oak Ridge National Laboratory. It gives a brief overview of research activities spanning the past 15 years that have sought to provide both an improved understanding of and a predictive capability for contaminant transport processes in highly structured, heterogeneous subsurface environments that are complicated by fracture flow and matrix diffusion. Our approach involved a multiscale (cm-to-ha) experimental and numerical endeavor to investigate coupled time-dependent hydrological and geochemical processes that control contaminant migration in unsaturated and saturated soil and rock. Novel tracer techniques and experimental manipulation strategies were applied at laboratory, intermediate, and field scales to unravel the influence of multiple processes on contaminant fate and transport. The basic research strategies have significantly improved our conceptual understanding of time-dependent solute migration in fractured subsurface media. This information has proven useful in decision-making processes regarding selection of effective remedial actions and interpretation of monitoring results after remediation is complete.
| Original language | English |
|---|---|
| Title of host publication | Dynamics of Fluids in Fractured Rock, 2000 |
| Editors | Paul A. Witherspoon, Boris Faybishenko, Sally M. Benson |
| Publisher | Blackwell Publishing Ltd |
| Pages | 389-400 |
| Number of pages | 12 |
| ISBN (Electronic) | 9781118669662 |
| ISBN (Print) | 9780875909806 |
| DOIs | |
| State | Published - 2000 |
Publication series
| Name | Geophysical Monograph Series |
|---|---|
| Volume | 122 |
| ISSN (Print) | 0065-8448 |
| ISSN (Electronic) | 2328-8779 |
Funding
Acknowledgments. This research was supported by the Environmental Technology Partnership (ETP) program of the Office of Biological and Environmental Research, U.S. Department of Energy. The authors would like to thank Mr. Paul Bayer, contract officer for DOE's ETP program, for financially supporting this research. Oak Ridge National Laboratory is managed by Lockheed Martin Energy Research Corporation for the U.S. Department of Energy, under contract DE-AC05-960R22464. Environmental Sciences Division, ORNL Publication No. 4951. This research was supported by the Environmental Technology Partnership (ETP) program of the Office of Biological and Environmental Research, U.S. Department of Energy. The authors would like to thank Mr. Paul Bayer, contract officer for DOE’s ETP program, for financially supporting this research. Oak Ridge National Laboratory is managed by Lockheed Martin Energy Research Corporation for the U.S. Department of Energy, under contract DE-AC05-960R22464. Environmental Sciences Division, ORNL Publication No. 4951.
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