Mean Radiation Force of Shear Plane Waves on a Sphere in an Elastic Medium

F. G. Mitri
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Abstract

The mean (time-averaged) longitudinal force component (i.e. acting along the direction of wave propagation) arising from the interaction of linearly-polarized plane progressive shear elastic waves, incident upon a sphere embedded in an elastic medium, is considered. Exact partial-wave series expansions are derived based on the integration of the radial component of the time-averaged elastodynamic Poynting vector in spherical coordinates. The method is verified stemming from the law of energy conservation applied to elastic scattering. The analytical modeling is useful and provides improved physical understanding of shear-to-compressional (S $\to $ P) mode conversion, as well as shear-to-shear (S $\to $ S) and transverse-to-transverse (T $\to $ T) mode preservation in the context of the mean elastic force. The elastic wave scattering formulation based on Debye’s shear and transverse potentials is solved first, and used subsequently to derive the mathematical expression of the mean force efficiency. Numerical computations illustrate the analysis with particular emphasis on the components related to mode preservation, coupling and conversion separately. It is shown here that the total force originates from individual interactions of scattering terms between the scattered pure shear (S $\to $ S) and transverse (T $\to $ T) waves, in addition to shear-to-transverse (S $\rightleftarrows $ T) coupling, and a shear-to-compression (S $\to $ P) mode conversion that contributes negligibly to the total mean force. The benchmark solution presented in this analysis for the time-averaged elastic force of shear plane progressive waves can be utilized to validate numerical methods (such as the FEM, BEM, FDTD or other). The results can provide a priori information for the optimization and design of experimental setups in various applications in biomedical ultrasound, elastography and elasticity imaging, shear-wave activation of implantable devices, characterization of biological tissue, seismology and other related applications in elastic wave scattering and radiation force.
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弹性介质中球面上剪切平面波的平均辐射力
考虑了入射到嵌入弹性介质中的球体上的线极化平面渐进剪切弹性波的相互作用所产生的平均(时间平均)纵向力分量(即沿波传播方向作用)。基于球坐标下时均弹性动力波印亭矢量径向分量的积分,导出了精确的分波级数展开式。从弹性散射的能量守恒定律出发,对该方法进行了验证。分析建模非常有用,并提供改善的物理理解shear-to-compressional (S P - \美元)模式转换,以及shear-to-shear(\美元年代)和transverse-to-transverse (T \美元T)模式上下文中的保护意味着弹性力。首先求解基于德拜剪切势和横向势的弹性波散射公式,然后推导平均力效率的数学表达式。数值计算说明了分析的结果,并分别对模态保持、耦合和转换三个部分进行了分析。这里显示的是总力源于个人交互之间的散射条件分散纯剪(\美元年代)和横向(T \美元T)波,除了shear-to-transverse \ rightleftarrows美元(S T)耦合,和shear-to-compression (S P - \美元)模式变换可忽视地有助于总意味着力量。本文提出的剪切面进行波时均弹性力基准解可用于验证数值方法(如FEM、边界元法、时域有限差分法等)。研究结果可为生物医学超声、弹性成像、可植入设备的剪切波激活、生物组织表征、地震学和其他相关应用中弹性波散射和辐射力的实验装置的优化和设计提供先验信息。
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