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通过位移势-拉普拉斯-汉克尔-卡尼亚尔变换法对内部荷载的时域半空间格林函数进行解析求解。

Analytic resolution of time-domain half-space Green's functions for internal loads by a displacement potential-Laplace-Hankel-Cagniard transform method.

作者信息

Pak Ronald Y S, Bai Xiaoyong

机构信息

Department of Civil, Environmental and Architectural Engineering, University of Colorado, Boulder, CO 80309-0428, USA.

出版信息

Proc Math Phys Eng Sci. 2020 Mar;476(2235):20190610. doi: 10.1098/rspa.2019.0610. Epub 2020 Mar 4.

Abstract

A refined yet compact analytical formulation is presented for the time-domain elastodynamic response of a three-dimensional half-space subject to an arbitrary internal or surface force distribution. By integrating Laplace and Hankel transforms into a method of displacement potentials and Cagniard's inversion concept, it is shown that the solution can be derived in a straightforward manner for the generalized classical wave propagation problem. For the canonical case of a buried point load with a step time function, the response is proved to be naturally reducible with the aid of a parametrized Bessel function integral representation to six wave-group integrals on finite contours in the complex plane that stay away from all branch points and the Rayleigh pole except possibly at the starting point of the contours. On the latter occasions, the possible singularities of the integrals can be rigorously extracted by an extended method of asymptotic decomposition, rendering the residual numerical computation a simple exercise. With the new solution format, the arrival time of each wave group is derivable by simple criteria on the contour. Typical results for the time-domain response for an internal point force as well as the degenerate case of a surface point source are included for comparison and illustrations.

摘要

针对三维半空间在任意内部或表面力分布作用下的时域弹性动力学响应,提出了一种精确而紧凑的解析公式。通过将拉普拉斯变换和汉克尔变换集成到位移势方法和卡尼亚尔反演概念中,结果表明,对于广义经典波传播问题,可以直接导出其解。对于具有阶跃时间函数的埋入点载荷的典型情况,借助参数化贝塞尔函数积分表示,证明响应可自然简化为复平面上有限轮廓上的六个波群积分,这些轮廓远离所有分支点和瑞利极点,可能除了轮廓的起点。在后一种情况下,积分的可能奇点可以通过渐近分解的扩展方法严格提取,从而使剩余的数值计算变得简单。利用新的解格式,每个波群的到达时间可以通过轮廓上的简单准则推导出来。给出了内部点力时域响应的典型结果以及表面点源的退化情况,用于比较和说明。

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本文引用的文献

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THE SEISMIC BURIED PULSE.地震掩埋脉冲。
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THE SEISMIC SURFACE PULSE.地震表面脉冲。
Proc Natl Acad Sci U S A. 1955 Jul 15;41(7):469-80. doi: 10.1073/pnas.41.7.469.

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