The authors present a second order explicit finite-difference scheme f
or elastic waves in 2-D nonhomogeneous media. These schemes are based
on integrating the equations of motion and the stress-free surface con
ditions across the discontinuities before discretizing them on a grid.
As an alternative for the free-surface treatment, a scheme using zero
density above the surface is suggested. This scheme is first order an
d is shown to be a natural consequence of the integrated equations of
motion and is called a vacuum formalism. These schemes remove instabil
ities encountered in earlier integration schemes. The consistency stud
y reveals a close link between the vacuum formalism and the integrated
/discretized stress-free condition, giving priority to the vacuum form
alism when a material discontinuity reaches the free surface. The two
presented free-surface treatments coincide in the sense of the limit (
grid size --> 0) for lateral homogeneity at or near the free surface.