The acoustic wave equation in two dimensions relates the spatial
derivatives to the time derivative. Using the acoustic approximation
the wave equation is derived in Section 4.
The dimensionality
of the equation requires a media velocity
, the
sound speed.
In the two dimensional model of Figure 1
the surface coordinate is
and the depth coordinate
is
with the positive axis down, a tradition in the oil industry.
This half space is defined for
and for a bounded
.
The pressure wave field is
and the seismic source is
.
The inhomogeneous constant density two dimensional
wave equation is
This equation is hyperbolic and the inhomogeneity is due to the
variable model velocities. The seismic source
is applied at or
near the surface. Sources are sometimes buried to improve the
signal strength and to reduce noise generated by the near
surface. Receivers are placed in a line parallel to the
expected principal dip of the subsurface.
This is done to reduce the energy scattering by out of plane
reflectors.
The rest of this chapter is organized in the following manner:
The seismic data are too complex to visualize as numbers so visualization tools are provided to help in understanding the modeling and imaging process.