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Published on: November 1, 2016
Mechanism for detecting NAPL using electrical resistivity imaging.
Todd Halihan1, Valina Sefa1, Tom Sale2
1School of Geology, Oklahoma State University, 105 Noble Research Center, Stillwater, OK, USA.
Electrical resistivity imaging (ERI) can detect non-aqueous phase liquids (NAPLs) in freshwater. A NAPL barrier mechanism, where thin NAPL layers block pore throats, generates detectable resistive signals, with 3.3cm thickness being a key threshold.
Area of Science:
- Environmental Geophysics
- Hydrogeology
- Contaminant Hydrogeology
Background:
- Electrical resistivity imaging (ERI) is used to detect non-aqueous phase liquid (NAPL) impacts in freshwater environments.
- The underlying mechanism generating the resistive signature of NAPLs during ERI remains poorly understood.
Purpose of the Study:
- To investigate the electrical barrier mechanism for detecting NAPLs using ERI.
- To develop a theoretical basis for the mechanism and validate it through laboratory experiments and modeling.
Main Methods:
- A two-dimensional sand tank experiment was conducted using ERI.
- Photographic techniques quantified petroleum saturation.
- Forward modeling was performed to simulate the laboratory experiment.
Main Results:
- The study confirmed that thin, saturated NAPL barriers can block pore throats, generating detectable electrical resistivity signals.
- NAPL thickness, not bulk volume, is critical; a threshold of 3.3cm NAPL thickness was identified for detectable resistivity changes (>3%).
- The maximum observed resistivity increase due to NAPL was 37%.
Conclusions:
- ERI can detect small quantities of NAPL if they form barriers of sufficient thickness.
- The primary mechanism for resistivity signal generation is a high-resistivity zone of separate-phase liquid blocking pore-scale current flow.
- Forward models validated the NAPL barrier mechanism theory for the experimental conditions.
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