Preprint Article Version 1 Preserved in Portico This version is not peer-reviewed

Effects of Background Porosity on Seismic Anisotropy in Fractured Rocks: An Experimental Study

Version 1 : Received: 20 June 2023 / Approved: 21 June 2023 / Online: 21 June 2023 (08:52:10 CEST)

A peer-reviewed article of this Preprint also exists.

Zhang, Y.; Di, B.; Gao, F.; Li, L. Effects of Background Porosity on Seismic Anisotropy in Fractured Rocks: An Experimental Study. Appl. Sci. 2023, 13, 8379. Zhang, Y.; Di, B.; Gao, F.; Li, L. Effects of Background Porosity on Seismic Anisotropy in Fractured Rocks: An Experimental Study. Appl. Sci. 2023, 13, 8379.

Abstract

Fractures are present in hydrocarbon reservoirs of different porosity ranges. Seismic anisotropy has been widely used in fracture characterization and shown to be sensitive to background matrix porosities in theoretical studies. An understanding of the effects of background porosity on seismic anisotropy could improve seismic characterization in different fractured reservoirs. Based on synthetic rocks with controlled fractures, we conducted laboratory experiments to investigate the influence background porosity has on P wave anisotropy and shear wave splitting. A set of rocks containing the same fracture density (0.06) with varying porosities of 15.3%, 22.1%, and 30.8% were constructed. P and S wave velocities were measured at 0.5 MHz as rocks were water saturated. Results show that when porosity increased from 15.3% to 22.1%, P wave anisotropy and shear wave splitting exhibit slight fluctuations. However, when porosity continued to increase to 30.8%, P wave anisotropy declined sharply while shear wave splitting stayed nearly constant. The measured results were compared with predictions from equivalent medium theories. Qualitative agreements were found between theoretical predictions and measured results. In Eshelby-Cheng model, the increase of porosity reduces the fracture-induced perturbation in the fracture normal direction, resulting in a lower P wave anisotropy. In Gurevich(2003) model, the increase of porosity can reduce the compressional stiffness in parallel direction to a larger extent than that in perpendicular direction, thus leading to lower P wave anisotropy.

Keywords

Anisotropy; Fractures; Porosity; Rock physics

Subject

Environmental and Earth Sciences, Geophysics and Geology

Comments (0)

We encourage comments and feedback from a broad range of readers. See criteria for comments and our Diversity statement.

Leave a public comment
Send a private comment to the author(s)
* All users must log in before leaving a comment
Views 0
Downloads 0
Comments 0
Metrics 0


×
Alerts
Notify me about updates to this article or when a peer-reviewed version is published.
We use cookies on our website to ensure you get the best experience.
Read more about our cookies here.