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Elastic Waves in Homogeneous and Layered Transversely-Isotropic Media: Gaussian Wave Packets and Green Functions

机译:均质和层状横观各向同性介质中的弹性波:高斯波包和格林函数

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摘要

The increasing use of composites and composite laminates requires extensive efforts in developing NDE methods for these sophisticated materials. The main problem, especially with respect to algorithmic imaging, arises from their anisotropic nature which causes the splitting of phase-and group velocity directions. Therefore the inverse scattering theory established for acoustic [1] or isotropic materials [2] does not sufficiently describe wave propagation and imaging in composites. In layered structures additional difficulties are associated with multiple reflection and transmission. Hence, for transversely-isotropic materials such as fiber-reinforced composites, we first discuss plane wave solutions of the elastodynamic equation of motion yielding slowness-and group velocity diagrams, using a coordinate-free approach as given in [3] for the electromagnetic case and in [4] for the isotropic case. The propagation of Gaussian wave packets in unidirectional homogeneous and layered structures is then calculated for arbitrary layer orientations; the results are shown as time domain wavefront snapshots. Finally, an integral representation of Green’s functions for the transversely-isotropic medium is given via spatial Fourier-transforms, being particularly convenient to provide the basis for imaging in terms of Diffraction Tomography [1]. All results are given for arbitrary fiber direction.
机译:复合材料和复合材料层压板的使用不断增加,需要在开发用于这些复杂材料的NDE方法方面付出大量的努力。主要问题,尤其是关于算法成像的主要问题是由于它们的各向异性而引起的,这导致了相速度和群速度方向的分裂。因此,为声学[1]或各向同性材料[2]建立的逆散射理论不足以描述复合材料中的波传播和成像。在分层结构中,附加的困难与多次反射和透射有关。因此,对于横向各向同性的材料,例如纤维增强复合材料,我们首先讨论电磁弹性情况下运动的弹性动力学方程的平面波解,从而产生慢度和群速度图,使用[3]中给出的无坐标方法。而在[4]中则是各向同性的情况。然后针对任意层方向计算高斯波包在单向均匀和分层结构中的传播。结果显示为时域波前快照。最后,通过空间傅立叶变换给出了横观各向同性介质的格林函数的积分表示,特别方便地提供了基于衍射层析成像技术的成像基础[1]。所有结果均针对任意纤维方向给出。

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