摘要
本文借助线性滑动理论,将裂隙密度、纵横比等不同物性参数等效为正交介质刚度矩阵,建立两组正交直立裂隙介质正演模型.利用基于最小二乘法优化的高精度交错网格高阶有限差分法模拟弹性波在正交介质中的传播过程.模拟结果表明介质各向异性强度与裂隙物性直接相关,正演波场和共炮点显示相比普通交错网格,最小二乘优化方法可以压制数值频散现象,明显提高模拟精度,子波主频较高和模型波速较低时改善效果更为突出.
In this paper, with the help of the linear slip theory, different physical parameters such as fracture density, aspect ratio are equivalent to stiffness matrix of orthorhombic medium, to establish forward model of two sets upright orthorhombic fractures. through high-precision staggered grid high-order finite difference, which is optimized by the least squares method, to simulate the propagation process of in this medium. The simulation results show that the anisotropy of the medium is directly related to the physical properties of fractures, forward wave field and common shot point gathers display that, compared to the original staggered grid, least squares method can be used to suppress the numerical dispersion phenomena, improve simulation accuracy significantly, the effect is more prominent when the wavelet frequency is high or the velocity of model is low.
作者
杜泽源
吴国忱
李雨生
DU Ze-yuan;WU Guo-chen;LI Yu-sheng(School of Geosciences,China University of Petroleum(East China),Shandong Qingdao 266580,China;Laboratory for Marine Mineral Resources,Qingdao National Laboratory for Marine Science and Technology,Shandong Qingdao 266580,China)
出处
《地球物理学进展》
CSCD
北大核心
2019年第1期69-79,共11页
Progress in Geophysics
基金
国家科技重大专项(2016ZX05024-001-008)
国家自然科学基金联合基金项目(U1562215)联合资助
关键词
正交各向异性
线性滑动理论
交错网格有限差分
最小二乘优化方法
频散压制
Orthorhombic anisotropy
Linear slip theory
Staggered grid finite difference
Least squares optimize method
Suppress dispersion