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Geophysical Institute
Slovak Academy of
Sciences
Dúbravská cesta 9
842 28 Bratislava, Slovak
Republic
(P. M., J. K.)
Department of Mathematics
Engineering Faculty
Slovak
Technical University
Nám. Slobody 17
812 31 Bratislava
Slovak
Republic
(L. H.)
We investigated stability and grid dispersion in the 3D fourth-order in space, second-order in time, displacement-stress staggered-grid finite-difference scheme. Though only displacement-stress scheme is explicitly treated, all results also apply to the velocity-stress and displacement-velocity-stress finite-difference schemes.
We derived independent stability conditions for the P and S waves by exact separation of equations for the two types of waves.
Since the S-wave group velocity can differ from the actual velocity as much as 5% for the sampling ratio 1/5 (that is usually used in modeling), we recommend to sample a minimum S wavelength by six grid spacings.
Grid dispersion is strongest for a wave propagating in the direction of a coordinate axis and weakest for a wave propagating along a body diagonal.
Grid dispersion in the fourth-order scheme for the sampling ratios s = 1/5 and s = 1/6 is smaller than grid dispersion in the second-order scheme for s = 1/10 and s = 1/12, respectively.
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