Abstract
A knowledge of wave propagation in boreholes with gas hydrate-bearing sediments, a typical three-phase porous medium, is of great significance for better applications of acoustic logging information on the exploitation of gas hydrate. To study the wave propagation in such waveguides based on the Carcione–Leclaire three-phase theory, according to the equations of motion and constitutive relations, a staggered-grid finite-difference time-domain (FDTD) scheme and a real axis integration (RAI) algorithm in a two-dimensional (2D) cylindrical coordinate system are proposed. In the FDTD scheme, the partition method is used to solve the stiff problem, and the nonsplitting perfect matched layer (NPML) scheme is extended to solve the problem of the false reflection waves from the artificial boundaries of the computational region. In the RAI algorithm, combined with six boundary conditions, the displacement potentials of waves are studied to calculate the borehole acoustic wavefields. The effectiveness is verified by comparing the results of the two algorithms. On this basis, the acoustic logs within a gas hydrate-bearing sediment are investigated. In particular, the wave field in a borehole is analyzed and the amplitude of a Stoneley wave under different hydrate saturations is studied. The results indicate that the attenuation coefficient of the Stoneley wave increases with the increase of gas hydrate saturation. The acoustic responses in a borehole embedded in a horizontally stratified hydrate formation are also simulated by using the proposed FDTD scheme. The result shows that the amplitude of the Stoneley wave from the upper interface is smaller than that from the bottom interface.
Highlights
Rosenbaum [19] first applied Biot’s theory [20,21,22,23,24,25] of porous media to the study of acoustic logging in a fluid-saturated porous formation and used the real axis integration (RAI) method to simulate the full waveform of the borehole excited by a monopole source, which is the beginning of the theoretical study on acoustic logging in porous media
To model the acoustic responses excited by an axisymmetric point source on the borehole axis of a gas hydrate-bearing sediment, we propose both a RAI algorithm and a 2D finite-difference time-domain (FDTD) scheme
A velocity–stress FDTD algorithm with a nonsplitting perfect matched layer to simulate acoustic wave propagation in the borehole surrounded by a gas hydrate-bearing sediment
Summary
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Rosenbaum [19] first applied Biot’s theory [20,21,22,23,24,25] of porous media to the study of acoustic logging in a fluid-saturated porous formation and used the RAI method to simulate the full waveform of the borehole excited by a monopole source, which is the beginning of the theoretical study on acoustic logging in porous media. Used the FDTD algorithm to simulate the wave propagation in a borehole within a porous medium and studied the characteristics of the Stoneley wave reflection These studies show that much research has been performed on the acoustic logs with a two-phase porous medium. To model the acoustic responses excited by an axisymmetric point source on the borehole axis of a gas hydrate-bearing sediment (three-phase porous medium), we propose both a RAI algorithm and a 2D FDTD scheme. The research findings can provide a theoretical basis and guidance in applying acoustic logging information for the exploration and evaluation of natural gas hydrate
Sign-in/Register to view highlights & summary Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
