SCATTERING OF SHEAR WAVES BY SPHERICAL OBSTACLES

@article{citeulike:1196544, abstract = {The problem of the scattering of plane S waves by a perfectly rigid, infinitely dense sphere is formulated. Calculations are made for the case in which the medium outside the sphere has a Poisson's ratio of . The range of sizes of obstacles used in the calculations includes radii very small compared with the wave length and radii comparable to the wave length. The scattered wave motions include a P mode and two S modes. One of the S modes has a formal correspondence to the SH mode of plane seismology; the other corresponds to the SV mode. At large distances from the obstacle the scattered P and S fields are computed together with the phase shifts in time occurring in all the components. For small obstacles, the scattered azimuthal S component is circularly symmetric; the scattered meridional S component diffraction pattern is generally elongated in the direction of propagation; the scattered P component is generally broadside to the direction of propagation.}, author = {Knopoff, Leon }, citeulike-article-id = {1196544}, doi = {10.1190/1.1438575}, journal = {Geophysics}, keywords = {elasticity, scattering}, number = {2}, pages = {209--219}, posted-at = {2007-03-29 17:56:20}, priority = {2}, publisher = {SEG}, title = {SCATTERING OF SHEAR WAVES BY SPHERICAL OBSTACLES}, url = {http://scitation.aip.org/getabs/servlet/GetabsServlet?prog=normal\&id=GPYSA7000024000002000209000001\&idtype=cvips\&gifs=yes}, volume = {24}, year = {1959} }

TY - JOUR ID - citeulike:1196544 L3 - citeulike-article-id:1196544 TI - SCATTERING OF SHEAR WAVES BY SPHERICAL OBSTACLES JF - Geophysics VL - 24 IS - 2 SP - 209 EP - 219 PB - SEG N2 - The problem of the scattering of plane S waves by a perfectly rigid, infinitely dense sphere is formulated. Calculations are made for the case in which the medium outside the sphere has a Poisson's ratio of . The range of sizes of obstacles used in the calculations includes radii very small compared with the wave length and radii comparable to the wave length. The scattered wave motions include a P mode and two S modes. One of the S modes has a formal correspondence to the SH mode of plane seismology; the other corresponds to the SV mode. At large distances from the obstacle the scattered P and S fields are computed together with the phase shifts in time occurring in all the components. For small obstacles, the scattered azimuthal S component is circularly symmetric; the scattered meridional S component diffraction pattern is generally elongated in the direction of propagation; the scattered P component is generally broadside to the direction of propagation. KW - elasticity KW - scattering AU - Knopoff, Leon PY - 1959/// UR - http://scitation.aip.org/getabs/servlet/GetabsServlet?prog=normal&id=GPYSA7000024000002000209000001&idtype=cvips&gifs=yes ER -