Pure qP-wave equation in VTI media based on approximate method of completing the square

Author(s):  
Kai Liang ◽  
Shangrao Sun ◽  
Danping Cao ◽  
Xingyao Yin
2015 ◽  
Vol 46 (4) ◽  
pp. 342-348
Author(s):  
Ho Seuk Bae ◽  
Wookeen Chung ◽  
Jiho Ha ◽  
Changsoo Shin

2005 ◽  
Vol 24 (6) ◽  
pp. 618-620 ◽  
Author(s):  
Jiaxiang Ren ◽  
Clive Gerrard ◽  
James Mcclean ◽  
Mikhail Orlovich

Geophysics ◽  
2012 ◽  
Vol 77 (5) ◽  
pp. T171-T186 ◽  
Author(s):  
Kenneth P. Bube ◽  
Tamas Nemeth ◽  
Joseph P. Stefani ◽  
Ray Ergas ◽  
Wei Liu ◽  
...  

We studied second-order wave propagation systems for vertical transversely isotropic (VTI) and tilted transversely isotropic (TTI) acoustic media with variable axes of symmetry that have their shear-wave speeds set to zero. Acoustic TTI systems are commonly used in reverse-time migration, but these second-order systems are susceptible to instablities appearing as nonphysical stationary noise growing linearly in time, particularly in variable-tilt TTI media. We found an explanation of the cause of this phenomenon. The instabilities are not caused only by the numerical schemes; they are inherent to the differential equations. These instabilities are present even in homogeneous VTI media. These instabilities are caused by zero wave speeds at a wide variety of wavenumbers — a direct consequence of setting the shear-wave speeds to zero — coupled with the second time derivative in these systems. Although the second-order isotropic wave equation allows smooth time-growing solutions, a larger class of time-growing solutions exists for the second-order acoustic TI systems, including nonsmooth solutions. Boundary conditions appear to be less effective in controlling these time-growing solutions than they are for the isotropic wave equation. These systems conserve an incomplete energy that does not prevent the instabilities. The corresponding steady-state systems are no longer elliptic differential equations and can have nonsmooth solutions that are related to the instabilities. We started initially with homogeneous VTI media, and then extended these results to heterogeneous variable-tilt TTI media. We also developed a second-order acoustic system for heterogeneous variable-tilt TTI media derived directly from the full-elastic system for heterogeneous variable-tilt TTI media. All second-order systems with a dispersion relation obtained by setting the shear-wave speeds to zero in the elastic dispersion relation allowed these nonphysical time-growing solutions; however, knowing the cause of these instabilities, it may be possible to prevent or control the activation of these solutions.


2005 ◽  
Author(s):  
Jiaxiang Ren ◽  
Clive Gerrard ◽  
James McClean ◽  
Mikhail Orlovich

2016 ◽  
Author(s):  
Guojie Song ◽  
Rong Huang ◽  
Jidong Tian ◽  
Yali Chen ◽  
Puchun Chen ◽  
...  
Keyword(s):  

2005 ◽  
Author(s):  
R.S. Day ◽  
F. Lui ◽  
D.W. Hanson ◽  
N.D. Whitmore ◽  
C.C. Mosher ◽  
...  

2005 ◽  
Vol 48 (2) ◽  
pp. 448-457 ◽  
Author(s):  
Li-Nong LIU ◽  
Hong-Wei GAO ◽  
Hong LIU ◽  
Jian-Feng ZHANG

2012 ◽  
Vol 588-589 ◽  
pp. 1380-1385
Author(s):  
Gui Hua Li ◽  
Jian Guo Feng ◽  
Nian Tian Lin ◽  
Gui Liang Li ◽  
Min Guo

A key issue in the wave equation simulation of seismic records is the boundary conditions. Due to computer memory and computation and other restrictions, can only be solved on a limited area, which will cause the introduction of an artificial reflector. So as to simulation of seismic wave propagation in an infinite medium, the boundary conditions must be constructed so that the interface of the reflection as little as possible. In 2.5D VTI media feature analysis absorbing boundary of higher order velocity-stress staggered-grid finite difference method are established. The mixed boundary of the feature analysis absorbing boundary plus damping attenuation condition is used in 2.5 D VTI numerical simulations, simulation results show that this method is an efficient absorption and attenuation boundary conditions.


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