Demonstrating Three-Dimensional Electrical Resistivity Imaging in Fractured Rock to Characterize Fractures and Monitor Amendment Injections

Tuesday, September 24, 2013: 9:50 a.m.
Judy Robinson , Earth & Environmental Sciences, Rutgers University, Newark, NJ
Lee D. Slater , Rutgers-Newark, Newark, NJ
Timothy Johnson , Energy and Environment Directorate, Pacific Northwest National Laboratory, Richland, WA
Dimitris Ntarlagiannis , Earth and Environmental Sciences, Rutgers University, Newark, NJ
Allen M. Shapiro , U.S. Geological Survey, Reston, VA
Claire R. Tiedeman , U.S. Geological Survey, Menlo Park, CA
Carole D. Johnson , Office of Groundwater, Branch of Geophysics, U.S. Geological Survey, Storrs, CT
Pierre J. Lacombe , U.S. Geological Survey, West Trenton, NJ
Frederick D. Day-Lewis , U.S. Geologic Survey, Storrs, CT
John W. Lane , Office of Groundwater, Branch of Geophysics, U.S. Geologic Survey, Storrs Mansfield, CT

Rutgers University, the U.S. Geological Survey, and Pacific Northwest National Laboratory are demonstrating the use of 3D cross-borehole electrical resistivity imaging (ERI) for improving the characterization of fractured rock aquifers and the monitoring of amendment treatments that biologically stimulate reductive dechlorination of chlorinated ethenes.  Seven, 4-inch diameter, boreholes have been drilled at the Naval Air Warfare Center (NAWC) in West Trenton, New Jersey, which is a mudstone fractured rock site contaminated with trichloroethylene, cis-1,2-dichloroethene, and vinyl chloride.  Interpretations of borehole geophysical logs including caliper, optical televiewer, acoustical televiewer, gamma, and ambient/transient heat pulse flowmeter determined local fracture locations, their hydraulic significance, and connectivity between boreholes.  Cross-hole hydraulic testing identified bedding-plane parting fracture zones and possible fault zones that are the dominant hydraulic pathways.  In a synthetic simulation based on the NAWC site, we found that constraining ERI inversions with this type of fracture zone information from geophysical logs and hydraulic testing substantially improved the resolution of fractures and the prediction of amendment transport away from the boreholes.  A field demonstration of ERI has been designed where 3D electrical resistance measurements were acquired from electrodes in all seven boreholes.  To test whether limiting the preferential current pathway introduced in a fluid-filled borehole will have a significant effect in resolving fracture zones in numerical modeling, highly resistive inflatable packers have been installed between two or more electrodes.  ERI measurements collected during a doublet tracer test will be used to: demonstrate the high-resolution capability of electrical resistivity in fractured rock, suggested in the synthetic studies, and to design an amendment injection for remediation.  Our goal is to demonstrate that ERI using structural constraints in numerical modeling improves characterization of fractures and spatial distribution of amendment treatments.

Judy Robinson, Earth & Environmental Sciences, Rutgers University, Newark, NJ
PhD Candidate in Near Surface Geophysics


Lee D. Slater, Rutgers-Newark, Newark, NJ
Lee Slater is an Associate Professor of Near Surface Geophysics at Rutgers University. He specializes in the application of electrical methods for investigating hydrogeological and microbial processes. Slater has co-authored 44 peer reviewed journal articles on near- surface geophysics, has served as Principal Investigator on more than 10 grant awards from federal agencies, is an Associate Editor of the American Geophysical Union (AGU) journal Water Resources Research, and currently serves as the Vice-Chair of the AGU Near Surface Geophysics Focus Group.


Timothy Johnson, Energy and Environment Directorate, Pacific Northwest National Laboratory, Richland, WA
Timothy Johnson is a research scientist for Pacific Northwest National Laboratory.


Dimitris Ntarlagiannis, Earth and Environmental Sciences, Rutgers University, Newark, NJ
Dimitris Ntarlagiannis is Assistant Professor in the Department of Earth and Environmental Sciences, Rutgers-Newark.


Allen M. Shapiro, U.S. Geological Survey, Reston, VA
Allen M. Shapiro is a Senior Research Hydrologist with the National Research Program of the U.S. Geological Survey in Reston, Virginia. His research focuses on the development of field techniques and methods of interpreting geologic, geophysical, hydraulic, and geochemical information in the characterization of fluid movement and chemical transport in fractured rock from meters to kilometers. Shapiro’s research has focused on a wide range of geologic environments, including crystalline and sedimentary rock, and carbonate aquifers that have undergone karstification. His research has been applied in issues of water supply, geotechnical engineering, waste isolation, and groundwater contamination and restoration.


Claire R. Tiedeman, U.S. Geological Survey, Menlo Park, CA
Claire Tiedeman is a Research Hydrologist at the U.S. Geological Survey, where her work involves characterizing and modeling flow and transport in fractured rock aquifers, calibrating and evaluating models of complex groundwater flow systems, and developing methods to evaluate prediction uncertainty. She is co-coordinator of USGS research on contaminant transport and remediation at the former Naval Air Warfare Center, and is co-author of the textbook Effective Groundwater Model Calibration: With Analysis of Data, Sensitivities, Predictions, and Uncertainty.


Carole D. Johnson, Office of Groundwater, Branch of Geophysics, U.S. Geological Survey, Storrs, CT
Carole Johnson has worked for the U.S. Geological Survey for 30 years and is a hydrologist with the Office of Groundwater, Branch of Geophysics in Storrs, Connecticut. Her research interests include integrated analysis and interpretation of hydraulic and borehole and surface geophysical data, and the use of geophysics to inform the design and implementation of hydrologic investigations.


Pierre J. Lacombe, U.S. Geological Survey, West Trenton, NJ
Pierre Lacombe is a hydrologist with the U.S. Geological Survey in West Trenton, New Jersey.


Frederick D. Day-Lewis, U.S. Geologic Survey, Storrs, CT
Frederick Day-Lewis is Research Hydrologist at the U.S. Geological Survey.


John W. Lane, Office of Groundwater, Branch of Geophysics, U.S. Geologic Survey, Storrs Mansfield, CT
John Lane is Chief, U.S. Geological Survey, Office of Ground Water, Branch of Geophysics