Journal cover Journal topic
Solid Earth An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 2.380 IF 2.380
  • IF 5-year value: 3.147 IF 5-year
    3.147
  • CiteScore value: 3.06 CiteScore
    3.06
  • SNIP value: 1.335 SNIP 1.335
  • IPP value: 2.81 IPP 2.81
  • SJR value: 0.779 SJR 0.779
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 32 Scimago H
    index 32
  • h5-index value: 31 h5-index 31
SE | Volume 10, issue 4
Solid Earth, 10, 1321–1336, 2019
https://doi.org/10.5194/se-10-1321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Solid Earth, 10, 1321–1336, 2019
https://doi.org/10.5194/se-10-1321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 08 Aug 2019

Research article | 08 Aug 2019

Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions

Simón Lissa et al.
Viewed  
Total article views: 773 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
559 205 9 773 43 20 11
  • HTML: 559
  • PDF: 205
  • XML: 9
  • Total: 773
  • Supplement: 43
  • BibTeX: 20
  • EndNote: 11
Views and downloads (calculated since 25 Mar 2019)
Cumulative views and downloads (calculated since 25 Mar 2019)
Viewed (geographical distribution)  
Total article views: 443 (including HTML, PDF, and XML) Thereof 440 with geography defined and 3 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Cited  
Saved (final revised paper)  
No saved metrics found.
Saved (discussion paper)  
No saved metrics found.
Discussed (final revised paper)  
No discussed metrics found.
Discussed (discussion paper)  
Latest update: 21 Jan 2020
Publications Copernicus
Download
Short summary
We quantify the effects that 3-D fractures with realistic distributions of aperture have on seismic wave attenuation and velocity dispersion. Attenuation and dispersion are caused by fluid pressure diffusion between the fractures and the porous background. We show that (i) both an increase in the density of contact areas and a decrease in their correlation length reduce attenuation and (ii) a simple planar fracture can be used to emulate the seismic response of realistic fracture models.
We quantify the effects that 3-D fractures with realistic distributions of aperture have on...
Citation