首页 | 本学科首页   官方微博 | 高级检索  
     检索      

分段光滑曲线边界波动方程数值模拟研究
引用本文:王忠仁,刘瑞,赵博雄.分段光滑曲线边界波动方程数值模拟研究[J].地球物理学报,2014,57(4):1199-1208.
作者姓名:王忠仁  刘瑞  赵博雄
作者单位:吉林大学仪器科学与电气工程学院地球信息探测仪器教育部重点实验室, 长春 130026
基金项目:国家自然科学基金项目(41074081)资助
摘    要:矩形网格有限差分法在地震波传播数值模拟方面具有计算速度快的显著优势,但该方法在处理复杂边界问题上存在着效率低的严重缺陷.本文针对分段光滑曲线边界定义了尖点处的一种正则导数,给出了矩形网格情形分段光滑曲线网格边界点法向导数的一种插值计算方法.采用矩形网格有限差分法对复杂边界地球介质模型进行地震波场数值模拟,并采用波场系列快照技术揭示地震波在起伏地表和复杂介质中的传播规律.模拟结果表明:法向导数插值计算方法为矩形网格有限差分法处理复杂边界提供了有效途径,采用波场系列快照技术可以清晰地展现地震波在反射界面的反射和透射规律、在尖点的绕射规律以及在自由表面的直达波和多次反射规律.

关 键 词:数值模拟  起伏地表  复杂地质体  有限差分法  分段光滑曲线边界  
收稿时间:2013-10-10

Numerical simulation of wave equation with segmented smooth curve boundaries
WANG Zhong-Ren,LIU Rui,ZHAO Bo-Xiong.Numerical simulation of wave equation with segmented smooth curve boundaries[J].Chinese Journal of Geophysics,2014,57(4):1199-1208.
Authors:WANG Zhong-Ren  LIU Rui  ZHAO Bo-Xiong
Institution:Key Lab of Geo-Exploration and Instrumentation, Ministry of Education, College of Instrumentation and Electrical Engineering, Jilin University, Changchun 130026, China
Abstract:The rectangular grid finite difference method in numerical simulation of seismic wave propagation possesses a significant advantage in fast computation speed. However, in dealing with complex boundaries this method has a serious defect of low efficiency. In this paper, a kind of regular derivative is defined for the cusp on a segmented smooth curve boundaries, and an interpolation method is given for computing normal derivatives at the rectangular grid points on the boundary. The finite difference method based on rectangular grids is used to simulate seismic wave propagation on an earth medium model with complex boundaries, and propagation laws in the relief surface and complex media are revealed using the technique of a series of wave field snapshots. The simulation results show that the normal derivative interpolation method provides an effective tool to deal with complex boundaries for the rectangular grid finite difference method, and the technique of the series of wave field snapshots can clearly reveal the reflection and transmission propagation laws on the reflective interface, the diffraction at a cusp as well as the direct wave and multiple reflection on the free surface.
Keywords:Numerical simulation  Relief surface  Complex geological body  Finite difference method  Segmented smooth curve boundary
本文献已被 CNKI 等数据库收录!
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号