1887

Abstract

Summary

The presence of multi-scaled fractures in the crust of the Earth has been largely evidenced by geological observations that support power laws to describe fracture distribution.

Two main approaches have been developed to study fractured media : numerical simulations of waves or effective medium theories that assumes an Elementary Representative Volume or ERV. Each of these methods focuses on a restricted range of fracture size because of computational or theoretical consideration.

In this work, the non-periodic homogenization is exploited to go beyond size restriction and explore the effective properties of multiscale fractured media. We first ensure that this method can be applied to various scales by comparing its solutions to those of the two previous approaches.

Then, we build a 2D medium that accommodates fractures of various lengths. The density of each fracture set is predicted by a power law function of the fracture size, as supported by geological studies. We evidenced that the non-periodic homogenization is efficient to retrieve the effective properties of fractured media and that this method is well adapted to investigate multiscale fractured medium.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.202011943
2021-10-18
2024-04-20
Loading full text...

Full text loading...

References

  1. Allegre, C. J., Le Mouel, J. L., & Provost, A.
    (1982). Scaling rules in rock fracture and possible implications for earthquake prediction. Nature, 297(5861), 47.
    [Google Scholar]
  2. Bonnet, E., Bour, O., Odling, N. E., Davy, P., Main, I., Cowie, P., & Berkowitz, B.
    (2001). Scaling of fracture systems in geological media. Reviews of geophysics, 39(3), 347–383.
    [Google Scholar]
  3. Capdeville, Y., Guillot, L., & Marigo, J. J.
    (2010). 2-D non-periodic homogenization to upscale elastic media for P-SV waves. Geophysical Journal International, 182(2), 903–922.
    [Google Scholar]
  4. Cho, Y., Gibson, R. L.Jr, Lee, J., & Shin, C.
    (2019). Linear-slip discrete fracture network model and multiscale seismic wave simulation. Journal of Applied Geophysics, 164, 140–152.
    [Google Scholar]
  5. Cupillard, P., & Capdeville, Y.
    (2018). Non-periodic homogenization of 3-D elastic media for the seismic wave equation. Geophysical Journal International, 213(2), 983–1001.
    [Google Scholar]
  6. Grechka, V., & Kachanov, M.
    (2006). Effective elasticity of fractured rocks: A snapshot of the work in progress. Geophysics, 71(6), W45–W58.
    [Google Scholar]
  7. Hudson, J. A.
    (1981). Wave speeds and attenuation of elastic waves in material containing cracks. Geophysical Journal International, 64(1), 133–150.
    [Google Scholar]
  8. Lapin, R. L., Kuzkin, V. A., & Kachanov, M.
    (2018). On the anisotropy of cracked solids. International Journal of Engineering Science, 124, 16–23.
    [Google Scholar]
  9. Sevostianov, I., & Kachanov, M.
    (2002). On elastic compliances of irregularly shaped cracks. International Journal of Fracture, 114(3), 245–257.
    [Google Scholar]
  10. Schoenberg, M.
    (1980). Elastic wave behavior across linear slip interfaces. The Journal of the Acoustical Society of America, 68(5), 1516–1521.
    [Google Scholar]
  11. (1983). Reflection of elastic waves from periodically stratified media with interfacial slip. Geophysical Prospecting, 31(2), 265–292.
    [Google Scholar]
  12. Sevostianov, I., & Kachanov, M.
    (2013). Non-interaction approximation in the problem of effective properties. In Effective properties of heterogeneous materials (pp. 1–95). Springer, Dordrecht.
    [Google Scholar]
  13. Vasilyeva, M., De Basabe, J. D., Efendiev, Y., & Gibson, R. L.Jr
    (2019). Multiscale model reduction of the wave propagation problem in viscoelastic fractured media. Geophysical Journal International, 217(1), 558–571.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.202011943
Loading
/content/papers/10.3997/2214-4609.202011943
Loading

Data & Media loading...

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