Let be displacement along the source line and let be its force per unit length. The shear-horizontal wave equation isRotational symmetry about the line makes . Integrate over a disk of radius and use the divergence theorem:At a fixed regular time, a logarithmic singularity and its time derivatives are locally integrable; the inertial integral is and vanishes as . The leading balance is consequently , giving the SH line-source near-field singularityThe reference length only changes the bounded term; boundary conditions and source history determine that term. This is a local fixed-time statement, interpreted distributionally in time if the source force has jumps. It establishes logarithmic spatial dependence directly, without extrapolating far-field ray spreading into the source.
Away from the line source, insert a leading wavefront form into the shear-horizontal wave equation and match the two most singular orders. The first gives the eikonal equation . The next givesEquivalently, SH ray-tube amplitude transport conserves , where is the transverse width of a two-dimensional ray tube. A line source has straight radial elastic rays and for fixed angular width, soThe same geometrical spreading applies to the first nonzero derivative discontinuity or leading wavefront singularity; the source history determines which waveform and normalization occur. In three dimensions a point source instead has and amplitude proportional to .
This does not contradict the SH line-source near-field singularity. Ray transport describes an arrival-front limit with small, or the high-frequency field outside the immediate source neighborhood. The logarithm describes at fixed elapsed time and includes the tail behind the two-dimensional wavefront. For example, a causal step force has the exact radial displacementFor , this is , the near-source logarithm. For with , it isThe coefficient of the leading arrival singularity therefore has exactly the ray-theory dependence. A force impulse gives the corresponding leading field. The limits describe different regions of one causal solution; neither is a uniform approximation to the other.
Choose interface , source in medium 1 and transmitted medium 2 at . Write , take to be signed tangential slowness, and defineThe propagating range is ; the absolute value is needed if both azimuthal directions are included. Snell law for elastic waves preserves . The incident ray reaches the interface after time at horizontal position , withIn the transmitted medium its velocity is . Therefore the refraction of a cylindrical SH wavefront givesTime is measured from source emission. For a later emission add its time to the clock. These straight transmitted rays and their common-time endpoints determine the refracted wavefront; critical incidence and an evanescent transmitted field are excluded by the strict slowness bound.
At a welded interface, elastic-interface boundary conditions require continuous SH displacement and shear traction. Incident and reflected vertical slownesses have signs , givingThus the local displacement coefficient isIt multiplies the leading waveform discontinuity as well as a harmonic displacement. At the interface the incident amplitude from SH ray-tube amplitude transport is , where is the incident path length and is the source normalization from the previous part.
The transmitted geometrical spreading is not simply its total path length. Differentiate the ray position with respect to at fixed travel time and project onto the unit direction transverse to the transmitted ray, . Since , the transverse width per unit isThe derivative of contributes only in the ray direction and drops out of this projection. At entry,Within uniform medium 2 the leading amplitude varies as , so the required refraction of a cylindrical SH wavefront amplitude isThe local transmission coefficient and ray-tube spreading together incorporate both impedance contrast and refraction. Indeed the normal energy transmission fraction is , while the change of transverse width supplies the refraction factor in the conserved tube flux. If the media coincide, and , reducing this expression to as required. The formula holds for the stated propagating slownesses, without a critical or head-wave contribution.
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