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常Q衰减介质分数阶波动方程优化有限差分模拟 被引量:5
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作者 孙成禹 乔志浩 +1 位作者 伍敦仕 滕腾 《地震学报》 CSCD 北大核心 2017年第3期343-355,共13页
本文基于Kjartansson常Q模型理论,推导了常Q衰减介质中黏声波和黏弹性波的速度-应力方程,并采用基于二项式窗函数的优化交错网格有限差分方法进行了数值模拟,同时引入不分裂的复频移卷积完全匹配层(CPML)吸收边界条件,以消除边界反射.... 本文基于Kjartansson常Q模型理论,推导了常Q衰减介质中黏声波和黏弹性波的速度-应力方程,并采用基于二项式窗函数的优化交错网格有限差分方法进行了数值模拟,同时引入不分裂的复频移卷积完全匹配层(CPML)吸收边界条件,以消除边界反射.使用基于自适应时间步长记忆方法的中心差分近似时间分数阶导数,与常用的短时记忆方法相比,提高了波动方程的离散化精度和计算效率.通过对比均匀模型下声波的数值解与解析解,验证了算法的精确性,并进一步分析了不同品质因子下地震波的频散及衰减特征.对BP盐丘模型的数值模拟结果可以较好地反映本文数值方法对复杂介质的适应性及频散压制效果. 展开更多
关键词 常Q衰减 分数阶导数 优化有限差分 自适应记忆 CPML
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时限时移相关法叠前逆时成像条件及其应用 被引量:13
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作者 陈可洋 《石油物探》 EI CSCD 北大核心 2011年第1期22-26,17,共5页
地震波逆时偏移法是目前成像精度最高的成像技术。分析了相关法叠前逆时成像的基本原理,提出了时限时移相关法叠前逆时成像条件。运用高阶交错网格有限差分法,按照一定的观测方式合成了基于Marmousi模型的123个炮集记录,并应用时限时移... 地震波逆时偏移法是目前成像精度最高的成像技术。分析了相关法叠前逆时成像的基本原理,提出了时限时移相关法叠前逆时成像条件。运用高阶交错网格有限差分法,按照一定的观测方式合成了基于Marmousi模型的123个炮集记录,并应用时限时移相关法叠前逆时成像条件进行了叠前逆时深度偏移,将获得的剖面与反射系数深度剖面进行了对比。数值计算结果表明,应用时限时移相关法叠前逆时成像条件获得的偏移剖面准确反映了Marmousi模型中的各个地质反射界面及其反射系数的变化特征。与时空移相关法叠前逆时成像条件相比,时限时移相关法叠前逆时成像条件能够大大减少计算量和存储量,提高了计算效率。 展开更多
关键词 时限时移相关法 叠前逆时深度偏移 MARMOUSI模型 高阶交错网格有限差分法 逆时成像条件
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Essential consistency of pressure Poisson equation method and projection method on staggered grids
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作者 王艺 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 2011年第6期789-794,共6页
A new pressure Poisson equation method with viscous terms is established on staggered grids. The derivations show that the newly established pressure equation has the identical equation form in the projection method. ... A new pressure Poisson equation method with viscous terms is established on staggered grids. The derivations show that the newly established pressure equation has the identical equation form in the projection method. The results show that the two methods have the same velocity and pressure values except slight differences in the CPU time. 展开更多
关键词 pressure Poisson equation projection method numerical analysis staggeredgrid computational fluid dynamics
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P-and S-wavefield simulations using both the firstand second-order separated wave equations through a high-order staggered grid finite-difference method
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作者 Chao-ying Bai Xin Wang Cai-xia Wang 《Earthquake Science》 2013年第2期83-98,共16页
In seismic exploration, it is common practice to separate the P-wavefield from the S-wavefield by the elastic wavefield decomposition technique, for imaging purposes. However, it is sometimes difficult to achieve this... In seismic exploration, it is common practice to separate the P-wavefield from the S-wavefield by the elastic wavefield decomposition technique, for imaging purposes. However, it is sometimes difficult to achieve this, especially when the velocity field is complex. A useful approach in multi-component analysis and modeling is to directly solve the elastic wave equations for the pure P- or S-wavefields, referred as the separate elastic wave equa- tions. In this study, we compare two kinds of such wave equations: the first-order (velocity-stress) and the second- order (displacement-stress) separate elastic wave equa- tions, with the first-order (velocity-stress) and the second- order (displacement-stress) full (or mixed) elastic wave equations using a high-order staggered grid finite-differ- ence method. Comparisons are given of wavefield snap- shots, common-source gather seismic sections, and individual synthetic seismogram. The simulation tests show that equivalent results can be obtained, regardless of whether the first-order or second-order separate elastic wave equations are used for obtaining the pure P- or S-wavefield. The stacked pure P- and S-wavefields are equal to the mixed wave fields calculated using the corre- sponding first-order or second-order full elastic wave equations. These mixed equations are computationallyslightly less expensive than solving the separate equations. The attraction of the separate equations is that they achieve separated P- and S-wavefields which can be used to test the efficacy of wave decomposition procedures in multi-com- ponent processing. The second-order separate elastic wave equations are a good choice because they offer information on the pure P-wave or S-wave displacements. 展开更多
关键词 Finite-difference method staggeredgrid First-order separate elastic wave equation Second-order separate elastic wave equation Multiple arrival tracking
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大地电磁倾子资料的三维正演研究 被引量:7
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作者 邓居智 蓝泽鸾 +1 位作者 陈辉 周峰 《地球物理学进展》 CSCD 北大核心 2015年第4期1666-1672,共7页
在实际复杂的三维地电条件下,倾子作为大地电磁法的重要解释参数之一,其正演模拟和响应分析对提高大地电磁法的探测精度具有重要作用.本文在简要阐述大地电磁三维正演基本理论的基础上,利用交错网格有限差分法开展了大地电磁三维倾子正... 在实际复杂的三维地电条件下,倾子作为大地电磁法的重要解释参数之一,其正演模拟和响应分析对提高大地电磁法的探测精度具有重要作用.本文在简要阐述大地电磁三维正演基本理论的基础上,利用交错网格有限差分法开展了大地电磁三维倾子正演模拟研究,首先正演模拟单个低、高阻两种地电模型的倾子响应,结果表明倾子资料能够较好反映地下异常体的空间分布;在此基础上,设计了含有两个低(高)阻异常体和低阻垂直断层的复杂组合模型并计算了其三维倾子响应,结果表明,倾子具有对复杂的地电结构良好的空间分辨率,且倾子响应既保留了模型中每单个异常体的倾子响应形态,又表现出了异常体之间相互作用的整体响应情况,进一步加深了对倾子的响应特征和规律、以及倾子资料对异常体边界的识别能力的认识,为倾子资料从定性解释向定量解释发展提供参考和依据. 展开更多
关键词 大地电磁测深 倾子 正演模拟 交错网格有限差分法
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Numerical solution of potential flow equations with a predictor-corrector finite difference method 被引量:2
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作者 Zhi-qiang LUO 《Journal of Zhejiang University-Science C(Computers and Electronics)》 SCIE EI 2012年第5期393-402,共10页
We develop a numerical solution algorithm of the nonlinear potential flow equations with the nonlinear free surface boundary condition.A finite difference method with a predictor-corrector method is applied to solve t... We develop a numerical solution algorithm of the nonlinear potential flow equations with the nonlinear free surface boundary condition.A finite difference method with a predictor-corrector method is applied to solve the nonlinear potential flow equations in a two-dimensional (2D) tank.The irregular tank is mapped onto a fixed square domain with rectangular cells through a proper mapping function.A staggered mesh system is adopted in a 2D tank to capture the wave elevation of the transient fluid.The finite difference method with a predictor-corrector scheme is applied to discretize the nonlinear dynamic boundary condition and nonlinear kinematic boundary condition.We present the numerical results of wave elevations from small to large amplitude waves with free oscillation motion,and the numerical solutions of wave elevation with horizontal excited motion.The beating period and the nonlinear phenomenon are very clear.The numerical solutions agree well with the analytical solutions and previously published results. 展开更多
关键词 Predictor-corrector method Nonlinear potential flow equations Finite difference method Staggered grid Nested iterative method
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