2022
DOI: 10.1029/2021jb023809
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Seismic Wave Propagation in Partially Saturated Rocks With a Fractal Distribution of Fluid‐Patch Size

Abstract: Laboratory experiments on partially saturated rocks show that seismic attenuation can be significant. The main mechanism, wave‐induced local fluid flow (WILFF), is affected by the spatial fluid distribution, especially in conditions of patchy saturation at different spatial scales. We propose a theory to obtain the seismic properties of partially saturated rocks based on fractal (self‐similar) patches, leading to an effective frequency‐dependent fluid modulus. The model combines the differential effective medi… Show more

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Cited by 34 publications
(10 citation statements)
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References 89 publications
(152 reference statements)
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“…To account for the effect of such distribution, the idea of fractal distributions and the differential effective medium (DEM) approach can be applied to extend our model, as that done in Zhang et al. (2021, 2022).…”
Section: Discussionmentioning
confidence: 99%
“…To account for the effect of such distribution, the idea of fractal distributions and the differential effective medium (DEM) approach can be applied to extend our model, as that done in Zhang et al. (2021, 2022).…”
Section: Discussionmentioning
confidence: 99%
“…As stated above, the understanding on wave-loss mechanisms of hydrate-bearing sediments is still limited (Best et al, 2013). Figure 3 shows the mechanisms considered in our triple-porosity model, i.e., local fluid flow between the rock skeleton and hydrate and clay frames, and the classical Biot global flow (Zhang et al, 2022).…”
Section: The Modelmentioning
confidence: 99%
“…A lot of rock physics models are available for simulating oil sands elastic properties (Guo and Han, 2016;Yuan et al, 2020;Qi et al, 2021;Zhang et al, 2021;Zhang et al, 2022). However, only three models (Hertz-Mindlin model, Voigt-Reuss-Hill average, and iso-frame model) are used here, mainly due to two reasons.…”
Section: Figure 14mentioning
confidence: 99%