WIT Inc. has the capability to efficiently and effectively simulate 3D seismic data in the acoustic limit, with a high quality pseudospectral modeling algorithm. Whether you want to model wide-azimuth marine data over your subsalt discovery, use areal shots over your land prospect to choose a survey design, or QC possible problems with an upcoming offset VSP, WIT Inc. can provide you with a high-quality solution.

Theoretically, finite difference approximation of the divergence should yield a faster algorithm than the pseudospectral method of computing the divergence in the Fourier domain. However, pseudospectral methods need only sample the wavefield at 2 grid points per wavelength, versus 3 points per wavelength with finite difference codes. Thus, for large models, finite difference algorithms may require domain decomposition over multiple CPUs, and efficiency never scales linearly with the number of CPUs.

Below we list some specifications of WIT's 3D Acoustic Wavefield Simulation algorithm:

• Can model marine, land, VSP, and OBC data
• Shots and receivers can exist on any topographic datum
• Simulates variable density as well as variable velocity
• Density field can be computed from velocity using Gardner's relation for sediments
• Predetermined table of stability information to fix optimum time step
• Simulates up to order 50 in time step - 4th order optimal in most cases
• Shots and receivers may lie between grid points

3D Synthetic Data Modeling over Topography

Click on any of the small images below to view the results of WIT's 3D Acoustic Wavefield Simulation of a synthetic 3D land survey over topography. The resultant data were then imaged with our 3D Shot Gather Migration algorithm. The data exhibit much scattering from topography, and the model has enough lateral velocity variation to keep any migration algorithm "honest".

Click on any thumbnail image above to start "slideshow"