首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Linear dynamic model for porous media saturated by two immiscible fluids
Institution:1. Mathematics and Physics College of Jiangsu University, Zhenjiang, Jiangsu 212013, PR China;2. Department of Earth Science, University of Bergen, Allegaten 41, N5007 Bergen, Norway;1. Laboratorio de Ingeniería de Reservorios, Instituto del Gas y del Petróleo, Facultad de Ingeniería, Universidad de Buenos Aires, Av. Las Heras 2214 Piso 3, C1127AAR Buenos Aires, Argentina;2. Instituto del Gas y del Petróleo, Facultad de Ingeniería, Universidad de Buenos Aires, CONICET, Argentina;3. Universidad de La Plata, Argentina;4. Department of Mathematics, Purdue University, 150 N. University Street, West Lafayette, IN 47907-2067, USA;5. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42c, 34010 Sgonico, Trieste, Italy
Abstract:A linear isothermal dynamic model for a porous medium saturated by two immiscible fluids is developed in the paper. In contrast to the mixture theory, phase separation is avoided by introducing one energy for the porous medium. It is an important advantage of the model based on one energy approach that it can account for the couplings between the phases. The volume fraction of each phase is characterized by the porosity of the porous medium and the saturation of the wetting phase. The mass and momentum balance equations are constructed according to the generalized mixture theory. Constitutive relations for the stress, pore pressure are derived from the free energy function. A capillary pressure relaxation model characterizing one attenuation mechanism of the two-fluid saturated porous medium is introduced under the constraint of the entropy inequality. In order to describe the momentum interaction between the fluids and the solid, a frequency independent drag force model is introduced. The details of parameter estimation are discussed in the paper. It is demonstrated that all the material parameters in our model can be calculated by the phenomenological parameters, which are measurable. The equations of motion in the frequency domain are obtained in terms of the Fourier transformation. In terms of the equations of motion in the frequency domain, the wave velocities and the attenuations for three P waves and one S wave are calculated. The influences of the capillary pressure relaxation coefficient and the saturation of the wetting phase on the velocities and attenuation coefficients for the four wave modes are discussed in the numerical examples.
Keywords:
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号