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首页> 外文期刊>Geosciences Journal >Two-point ray tracing in dipping layered media with constant or linearly varying velocity function
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Two-point ray tracing in dipping layered media with constant or linearly varying velocity function

机译:具有恒定或线性变化速度函数的浸入分层介质中的两点射线追踪

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摘要

A stable and accurate computational method is introduced for two-point ray tracing in the dipping layered media with constant or linearly varying vertical velocity distributions. This method is similar to the method introduced by Kim and Baag (2002) in horizontally layered media except that the slowness of a ray through whole ray path does not conserve due to dipping layers. The take-off angle at the source can be determined by the two-point ray tracing in the dipping layered media and can be described with respect to the horizontal distance between source and receiver. An equation of the horizontal distance can be obtained from the equations of ray paths and of interfaces in a nonlinear form. This nonlinear equation is expanded in a Taylor series with terms up to the second order about initial take-off angle of the ray for two-point ray tracing. This expansion yields the quadratic equation with respect to correction angle, which is the angular difference between the true and calculated take-off angle at the source. In this study, the initial take-off angle is basically estimated by applying the method introduced by Kim and Baag (2002). The computational results show stable and accurate two-point ray tracing for several models which include low velocity layer and producing triplication (or more) zone. Therefore, the accuracy and convergence rate of this method are sufficient enough to apply the method to a wide varieties of seismic problems.
机译:介绍了一种稳定且准确的计算方法,用于在垂直速度分布恒定或线性变化的浸渍层介质中进行两点射线跟踪。此方法类似于Kim和Baag(2002)在水平分层介质中引入的方法,不同之处在于,由于浸入层而无法保留通过整个光线路径的光线慢度。源处的起飞角可以通过浸入分层介质中的两点射线跟踪确定,并且可以相对于源和接收器之间的水平距离进行描述。可以从射线路径方程和非线性界面的方程获得水平距离方程。对于两点射线追踪,此非线性方程式以泰勒级数展开,其项直至射线的初始起飞角均达到二阶。这种扩展产生关于校正角的二次方程,校正角是在源头处真实的和计算的起飞角之间的角度差。在这项研究中,初始起飞角基本上是通过应用Kim和Baag(2002)引入的方法估算的。计算结果表明,对于包括低速层和产生三重(或更多)区域的几种模型,稳定,准确的两点射线追踪。因此,该方法的准确性和收敛速度足以将其应用于各种地震问题。

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