Modeling of the acoustoseismic induction process

The paper is devoted to modeling of the acoustoseismic induction process caused by the interaction of a harmonic wave with elastic half-space. This effect was first detected in experiments with powerful vibrational sources of seismic waves, carried out at the vibroseismic test site of Siberian Branch of RAS. The 2D problem of the elastic surface wave propagation with good allowance for the influence of an acoustic wave as boundary conditions is considered. The amplitude and the polarization characteristics of the induced surface wave and their dependence on elastic constants of the half-space are defined.