3D Time-Lapse Electrical Resistivity Imaging of Rock Damage Patterns and Gas Flow Paths Resulting from Two Underground Chemical Explosions

Journal Article · 27 November 2022 · Pure and Applied Geophysics

DOI: https://doi.org/10.1007/s00024-022-03165-y · OSTI ID:1900066

Johnson, Tim C. ; Knox, H. A.; Strickland, C.; Johnson, C.; Lowrey, J.; Sprinkle, D. P.; Linneman, D.; Vermeul, V.; Robey, E.; Chojnicki, K.; Ingraham, M.; Feldman, J.; Miley, H.

Abstract Rock damage from underground nuclear explosions (UNEs) has a strong influence on sub-surface gas movement and on seismic waveform characteristics, both of which are used to detect UNEs. Although advanced numerical simulation capabilities exist to predict rock damage patterns and corresponding detection signals, those predictions are dependent on (generally) unknown properties of the host rock. For example, the effects of in-situ mechanical heterogeneities on the explosively generated damage/fractures that provide gas flow pathways to the surface are not well understood, due largely to the difficulty in accessing and characterizing the near-source region. In this paper we demonstrate the emerging use of electrical resistivity tomography (ERT) for imaging rock damage and gas flow patterns resulting from two relatively small-scale underground chemical explosions. Pre-explosion ERT and crosshole seismic imaging revealed a natural fracture zone within the test bed. Post-explosion imaging revealed that the damage zone was non-symmetric and was focused primarily within the pre-existing fracture zone, located 10 m above the first explosion and 5 m above the second explosion. Time-lapse ERT imaging of heated air injected into the detonation borehole revealed the primary gas flow paths to be within the upper margin of the same primary damage zone. These results point to the utility of ERT imaging for understanding rock damage and gas flow patterns under experimental conditions, and to the importance of understanding the effects of geologic heterogeneity on UNE detection signals, particularly gas surface breakthrough times.

• Research Organization: Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
• Sponsoring Organization: USDOE National Nuclear Security Administration (NNSA), Office of Defense Nuclear Nonproliferation
• Grant/Contract Number: AC05-76RL01830
• OSTI ID: 1900066
• Report Number(s): PNNL-SA--169928; PII: 3165
• Journal Information: Pure and Applied Geophysics, Journal Name: Pure and Applied Geophysics Journal Issue: 4 Vol. 180; ISSN 0033-4553
• Publisher: Springer Science + Business MediaCopyright Statement
• Country of Publication: Switzerland
• Language: English