1887
24th International Geophysical Conference and Exhibition – Geophysics and Geology Together for Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

We present models of random resistor networks to relate electrical resistivity to fracture permeability in the upper crust. In this approach, the upper crust is modelled as a network of resistors that are randomly assigned to be either electrically and hydraulically conductive or resistive based on a network-wide probability of connection. In the models presented here, the conductive resistors are assigned resistance values based on a constant fracture diameter of 1 mm and a fluid resistivity of 0.1 Ωm, with variable fault length distributions and probabilities of connection. We have found that the permeability is very sensitive to both of these parameters, increasing to 8.33 × 108 times the matrix permeability in the fully connected case. The resistivity is less sensitive, increasing by a factor of 1000.

Loading

Article metrics loading...

/content/journals/10.1071/ASEG2015ab017
2015-12-01
2026-01-15
Loading full text...

Full text loading...

References

  1. Archie, G., 1942. The electrical resistivity log as an aid in determining some reservoir characteristics, Petroleum Transactions of the Australian Institute of Mining, Metallurgical, and Petroleum Engineers, 146, 54-62.
  2. Babadagli, T., Al-Salmi, S., et al., 2004. A review of permeability-prediction methods for carbonate reservoirs using well-log data, SPE Reservoir Evaluation & Engineering, 7(02), 75-88.
  3. Bahr, K., 1997. Electrical anisotropy and conductivity distribution functions of fractal random networks and of the crust: the scale effect of connectivity, Geophysical Journal International, 130(3), 649-660.
  4. Barnett, P. & Evans, T., 2010. Exploration and assessment of Hot Sedimentary Aquifer (HSA) geothermal resources in the Otway Basin Victoria, in Proceedings of the 2010 Australian Geothermal Energy Conference, Record 2010/35, pp. 106-111, Geoscience Australia.
  5. Brown, S. R.: Transport of fluid and electric current through a single fracture, Journal of Geophysical Research: Solid Earth, 94, (1989), 9429-9438.
  6. Hogarth, R., Holl, H., & McMahon, A., 2013. Flow testing results from Habanero EGS project, in Proceedings of the 2013 Australian Geothermal Energy Conference. Munoz, G., 2014. Exploring for geothermal resources with electromagnetic methods, Surveys in Geophysics, 35(1), 101122.
  7. Peacock, J., Thiel, S., Heinson, G., & Reid, P., 2013. Time-lapse magnetotelluric monitoring of an enhanced geothermal system, Geophysics, 78(3), B121-B130. Peacock, J. R., Thiel, S., Reid, P., & Heinson, G., 2012. Magnetotelluric monitoring of a fluid injection: Example from an enhanced geothermal system, Geophysical Research Letters, 39(18), 1-5.
  8. Pellerin, L., Johnston, J. M., & Hohmann, G. W., 1996. A numerical evaluation of electromagnetic methods in geothermal exploration, Geophysics, 61(1), 121-130.
  9. Reid, P. & Messeiller, M., 2013. Paralana Engineered Geothermal Systems project 3.5MW development plan, in Proceedings of the 2013 Australian Geothermal Energy Conference.
/content/journals/10.1071/ASEG2015ab017
Loading
  • Article Type: Research Article
Keyword(s): electromagnetic; permeability; resistivity
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error