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以共反射点为目标的二维射线追踪方法研究

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射线追踪方法是在假定地下地层为均匀、连续、层状介质的基础上,利用惠更斯原理、费马原理和斯奈尔定律来计算激发点到接收点的传播路径的方法.当前主流的设计软件射线追踪模块也是基于激发点到接收点的路径计算而编程模拟的.由于常用的射线追踪方法不是基于目标地层的,仅有少数模型软件可以查看指定层段的射线路径,主流设计软件射线追踪模块不能明确给出反射点的有效覆盖次数和确定共反射点(CRP)炮集.为此,在地震波射线传播理论的基础上,研究人员提出了以激发点或接收点为起始点,以共反射点为目标的射线追踪方法,并利用Matlab编程计算不同反射点位置的有效覆盖次数、炮集,用于指导激发点优化,进而实现二维勘探目的层的较均匀采样.
2D ray-tracing method analysis targeting common reflection points
The ray-tracing Method is the method that assumes underground layers are uniform,continuous,and layered me-dium,using Huygens-Fresnel principle,Fermat's principle,Snell's law to calculate the ray path from shots to receivers.The ray-tracing module of mainstream design software also relies on the ray path calculation from shots to receivers to program and sim-ulate.However,as the common ray tracing method is not based on the target layers,only a little model simulation software could show the ray path of the dedicated layer section.The mainstream design software could not show the effective fold cover-age of the dedicated reflection points and CRP shot gathering.Therefore,based on seismic wave ray propagation theory,re-searchers proposed the ray tracing method,taking shots or receivers as start and CRP as targets,and then programming with MATLAB to calculate the effective fold coverage,shot gather of different reflection points,guide the shots optimization,achieve more uniform sampling of the 2D exploration target layers.

effective Foldsray Tracingmultivariate nonlinear equationssource optimization

刘军胜

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中石化地球物理有限公司,北京 100000

有效覆盖次数 射线追踪 多元非线性方程组 激发点优化

2024

物探化探计算技术
成都理工大学 中国地质科学院物化探研究所

物探化探计算技术

CSTPCD
影响因子:0.398
ISSN:1001-1749
年,卷(期):2024.46(1)
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