In this paper, we consider numerical simulation of wave propagation in fluidsaturated porous media. A wavelet finite-difference method is proposed to solve the 2-D elastic wave equation. The algorithm combines flexibi...In this paper, we consider numerical simulation of wave propagation in fluidsaturated porous media. A wavelet finite-difference method is proposed to solve the 2-D elastic wave equation. The algorithm combines flexibility and computational efficiency of wavelet multi-resolution method with easy implementation of the finite-difference method. The orthogonal wavelet basis provides a natural framework, which adapt spatial grids to local wavefield properties. Numerical results show usefulness of the approach as an accurate and stable tool for simulation of wave propagation in fluid-saturated porous media.展开更多
基金the National Natural Science Foundation of China(No.40774056)Program of Excellent Team in Harbin Institute of Technology
文摘In this paper, we consider numerical simulation of wave propagation in fluidsaturated porous media. A wavelet finite-difference method is proposed to solve the 2-D elastic wave equation. The algorithm combines flexibility and computational efficiency of wavelet multi-resolution method with easy implementation of the finite-difference method. The orthogonal wavelet basis provides a natural framework, which adapt spatial grids to local wavefield properties. Numerical results show usefulness of the approach as an accurate and stable tool for simulation of wave propagation in fluid-saturated porous media.
文摘长波地波传播时延是决定陆基导航定位系统精度的关键,时域有限差分(Finite Difference-Time Domain,FDTD)方法可以提高其精度。但是FDTD方法在计算长距离的模型问题时迭代次数随之增多导致数值计算误差变大。主要通过基于圆柱坐标系下采用具有紧支撑特性的二阶矩Daubechies小波函数为尺度函数的时域多分辨分析(Multiresolution Time Domain,MRTD)方法来提高数值计算精度。随后对MRTD方法进行色散分析,最后将该方法应用于低频地波的传播预测中,提取观测点的衰减因子相位,与使用FDTD数值算法得到的结果进行对比,结果表明:MRTD方法可以在保持精度的前提下用时比FDTD更短。
