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横向各向同性介质拟声波一阶速度—应力方程 被引量:5
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作者 徐文才 杨国权 +1 位作者 李振春 李河昭 《石油地球物理勘探》 EI CSCD 北大核心 2016年第1期87-96,20,共10页
基于弹性波的基本理论,首先推导了VTI介质拟声波一阶速度—应力方程,通过坐标变换,还得到了TTI介质拟声波一阶速度—应力方程,并从能量守恒的角度证明了上述方程比基于频散关系推导出的拟声波方程更加稳定。针对各向异性参数ε<δ的... 基于弹性波的基本理论,首先推导了VTI介质拟声波一阶速度—应力方程,通过坐标变换,还得到了TTI介质拟声波一阶速度—应力方程,并从能量守恒的角度证明了上述方程比基于频散关系推导出的拟声波方程更加稳定。针对各向异性参数ε<δ的模型,对新推导的方程引入横波项,消除了残留的横波产生的数值模拟不稳定现象。通过对均匀二维模型和逆冲模型的正演模拟表明:新推导的方程不仅能很好地维持qP波的运动学特征,而且能够很好地适应任意旋转角度的TTI模型,并且在旋转角变化的TTI介质中数值稳定性要好于基于频散关系推导出的拟声波方程。 展开更多
关键词 TI介质 声学近似 速度—应力方程 拟声波方程 坐标变换 稳定性分析
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非均匀弹性介质地震波场伪谱法正演模拟 被引量:2
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作者 逄硕 刘财 《世界地质》 CAS CSCD 2014年第4期934-939,共6页
基于一阶速度—应力弹性波波动方程,利用傅里叶变换将空间导数变换到频率域求解,对介质波场进行正演模拟。本文结合实际勘探中可能存在的地质问题,设计了多种地质模型,包括背斜模型、向斜模型、透镜体模型和断层--侵入体模型等,进行了... 基于一阶速度—应力弹性波波动方程,利用傅里叶变换将空间导数变换到频率域求解,对介质波场进行正演模拟。本文结合实际勘探中可能存在的地质问题,设计了多种地质模型,包括背斜模型、向斜模型、透镜体模型和断层--侵入体模型等,进行了伪谱法地震波场正演模拟、合成地震记录的实现,并分析了其波场动力学变化特征。结果表明,应用伪谱法对复杂模型的模拟有较高的精度和可靠性,可直接用于辅助地震野外工作设计、反演解释和资料解释等工作。 展开更多
关键词 非均匀弹性介质 正演数值模拟 速度—应力方程 伪谱法 地质模型
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A study of perfectly matched layers for joint multicomponent reverse-time migration 被引量:3
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作者 杜启振 秦童 +1 位作者 朱钇同 毕丽飞 《Applied Geophysics》 SCIE CSCD 2010年第2期166-173,194,195,共10页
Reverse-time migration in finite space requires effective boundary processing technology to eliminate the artificial truncation boundary effect in the migration result.On the basis of the elastic velocity-stress equat... Reverse-time migration in finite space requires effective boundary processing technology to eliminate the artificial truncation boundary effect in the migration result.On the basis of the elastic velocity-stress equations in vertical transversely isotropic media and the idea of the conventional split perfectly matched layer(PML),the PML wave equations in reverse-time migration are derived in this paper and then the high order staggered grid discrete schemes are subsequently given.Aiming at the"reflections"from the boundary to the computational domain,as well as the effect of seismic event's abrupt changes at the two ends of the seismic array,the PML arrangement in reverse-time migration is given.The synthetic and real elastic,prestack,multi-component,reverse-time depth migration results demonstrate that this method has much better absorbing effects than other methods and the joint migration produces good imaging results. 展开更多
关键词 perfectly matched layer(PML) absorbing boundary reverse-time migration velocity-stress equation MULTI-COMPONENT
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Numerical modeling of seismic wavefields in transversely isotropic media with a compact staggered-grid finite difference scheme 被引量:7
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作者 杜启振 李宾 侯波 《Applied Geophysics》 SCIE CSCD 2009年第1期42-49,103,共9页
To deal with the numerical dispersion problem, by combining the staggeredgrid technology with the compact finite difference scheme, we derive a compact staggered- grid finite difference scheme from the first-order vel... To deal with the numerical dispersion problem, by combining the staggeredgrid technology with the compact finite difference scheme, we derive a compact staggered- grid finite difference scheme from the first-order velocity-stress wave equations for the transversely isotropic media. Comparing the principal truncation error terms of the compact staggered-grid finite difference scheme, the staggered-grid finite difference scheme, and the compact finite difference scheme, we analyze the approximation accuracy of these three schemes using Fourier analysis. Finally, seismic wave numerical simulation in transversely isotropic (VTI) media is performed using the three schemes. The results indicate that the compact staggered-grid finite difference scheme has the smallest truncation error, the highest accuracy, and the weakest numerical dispersion among the three schemes. In summary, the numerical modeling shows the validity of the compact staggered-grid finite difference scheme. 展开更多
关键词 transversely isotropic medium compact staggered-grid the first-order velocitystress wave equations numerical dispersion wave field simulation
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