The one-way acoustic wave equations can be derived, using eigenvalue d
ecomposition of the two-way wave equation in the Fourier domain, in su
ch a manner that the source term and the free-surface boundary conditi
on are explicitly introduced. The proposed form of the one-way wave eq
uations is well adapted to seismic reflection modeling because it allo
ws a pressure field recorded at the surface to be extrapolated directl
y in depth. A numerical example illustrates the appropriate implementa
tion of the source term and the free-surface boundary conditions. A co
mparison with a two-way modeling shows a good agreement of the compute
d wavefields.