Ivakin A N, Jackson D R
Andreev Acoustics Institute, Moscow, Russia.
J Acoust Soc Am. 1998 Jan;103(1):346-54. doi: 10.1121/1.421094.
It is known that marine sediments can support both compressional and shear waves. However, published work on scattering from irregular elastic media has not examined the influence of shear on sea bed scattering in detail. A perturbation model previously developed by the authors for joint roughness-volume scattering is used to study the effects of elasticity for three sea bed types: sedimentary rock, sand with high shear speed, and sand with "normal" shear wave speed. Both bistatic and monostatic cases are considered. For sedimentary rock it is found that shear elasticity tends to increase the importance of volume scattering and decrease the importance of roughness scattering relative to the fluid case. Shear effects are shown to be small for sands.
众所周知,海洋沉积物能够支持压缩波和剪切波。然而,已发表的关于不规则弹性介质散射的研究尚未详细考察剪切对海床散射的影响。作者先前开发的用于联合粗糙度 - 体积散射的微扰模型被用于研究三种海床类型(沉积岩、具有高剪切速度的沙子以及具有“正常”剪切波速度的沙子)的弹性效应。同时考虑了双基地和单基地情况。对于沉积岩,研究发现相对于流体情况,剪切弹性往往会增加体积散射的重要性并降低粗糙度散射的重要性。结果表明,剪切效应对于沙子来说较小。