دورية أكاديمية
Fluid pressure diffusion effects on the excess compliance matrix of porous rocks containing aligned fractures
| العنوان: | Fluid pressure diffusion effects on the excess compliance matrix of porous rocks containing aligned fractures |
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| المؤلفون: | Castromán, Gabriel Alejandro, Barbosa, Nicolás D., Rubino, Jorge German, Zyserman, Fabio Ivan, Holliger, Klaus |
| بيانات النشر: | Wiley Blackwell Publishing, Inc |
| المجموعة: | CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
| مصطلحات موضوعية: | ACOUSTIC PROPERTIES, FRACTURE AND FLOW, NUMERICAL APPROXIMATIONS AND ANALYSIS, WAVE PROPAGATION, https://purl.org/becyt/ford/1.5Test, https://purl.org/becyt/ford/1Test |
| الوصف: | The presence of sets of open fractures is common in most reservoirs, and they exert important controls on the reservoir permeability as fractures act as preferential pathways for fluid flow. Therefore, the correct characterization of fracture sets in fluid-saturated rocks is of great practical importance. In this context, the inversion of fracture characteristics from seismic data is promising since their signatures are sensitive to a wide range of pertinent fracture parameters, such as density, orientation and fluid infill. The most commonly used inversion schemes are based on the classical linear slip theory (LST), in which the effects of the fractures are represented by a real-valued diagonal excess compliance matrix. To account for the effects of wave-induced fluid pressure diffusion (FPD) between fractures and their embedding background, several authors have shown that this matrix should be complex-valued and frequency-dependent. However, these approaches neglect the effects of FPD on the coupling between orthogonal deformations of the rock. With this motivation, we considered a fracture model based on a sequence of alternating poroelastic layers of finite thickness representing the background and the fractures, and derived analytical expressions for the corresponding excess compliance matrix. We evaluated this matrix for a wide range of background parameters to quantify the magnitude of its coefficients not accounted for by the classical LST and to determine how they are affected by FPD. We estimated the relative errors in the computation of anisotropic seismic velocity and attenuation associated with the LST approach. Our analysis showed that, in some cases, considering the simplified excess compliance matrix may lead to an incorrect representation of the anisotropic response of the probed fractured rock. ; Fil: Castromán, Gabriel Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de ... |
| نوع الوثيقة: | article in journal/newspaper |
| وصف الملف: | application/pdf |
| اللغة: | English |
| تدمد: | 0956-540X 1365-246X |
| العلاقة: | info:eu-repo/semantics/altIdentifier/url/https://academic.oup.com/gji/article-abstract/222/1/715/5825648Test; http://hdl.handle.net/11336/140844Test; Castromán, Gabriel Alejandro; Barbosa, Nicolás D.; Rubino, Jorge German; Zyserman, Fabio Ivan; Holliger, Klaus; Fluid pressure diffusion effects on the excess compliance matrix of porous rocks containing aligned fractures; Wiley Blackwell Publishing, Inc; Geophysical Journal International; 222; 1; 7-2020; 715-733; CONICET Digital; CONICET |
| الإتاحة: | https://doi.org/10.1093/gji/ggaa197Test http://hdl.handle.net/11336/140844Test |
| حقوق: | info:eu-repo/semantics/restrictedAccess ; https://creativecommons.org/licenses/by-nc-sa/2.5/arTest/ |
| رقم الانضمام: | edsbas.95067AF0 |
| قاعدة البيانات: | BASE |
| تدمد: | 0956540X 1365246X |
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