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

基于共轭梯度法的全波形反演
引用本文:林朋,彭苏萍,卢勇旭,汪滔滔.基于共轭梯度法的全波形反演[J].煤田地质与勘探,2017,45(1):131.
作者姓名:林朋  彭苏萍  卢勇旭  汪滔滔
基金项目:国家重点研发计划课题(2016YFC0501102);国家自然基金煤炭联合基金项目(U1261203);山西省煤层气联合研究基金资助项目(2013012001)
摘    要:全波形反演是一种全新的地震成像方法,主要利用全波形信息反演地下介质参数,通过非线性优化波场理论值和观测值的残差实现波形反演。基于时间域声波方程,建立了时间域波场残差目标函数,以分层模型为例,分别从波场精度、目标函数收敛性和运行时间3个方面,比较了共轭梯度(Conjugate Gradient,CG)算法和拟牛顿算法(Broyden-Fletcher-Goldfarb-Shanno,BFGS)反演的效果。同时,应用共轭梯度法对正、逆断层模型和Marmousi模型进行了速度结构反演。反演结果表明:共轭梯度法计算效率较高,反演得到的速度模型精度更高,反演效果较好,是一种有效的波形反演方法。 

关 键 词:全波形反演    共轭梯度法    BFGS    声波方程
收稿时间:2015-12-15

Full waveform inversion based on the conjugate gradient method
Abstract:Full waveform inversion is a new seismic imaging method, which mainly uses full waveform information to inverse parameters of medium in the subsurface, and realizes waveform inversion by minimizing the residual between observed wavefield and theoretical wavefield using nonlinear optimization methods. The objective function of wavefield residual was established based on time domain acoustic wave equation. To test the capability of conjugate gradient(CG) algorithm and BFGS Quasi-Newton algorithm, waveform inversion was applied to a hierarchical model. The inversion effect was compared from wavefield precision, objective function convergence and running time respectively. The CG method was used to reconstruct velocity model on positive, reverse fault and Marmousi models. The inversion results show that the CG method has higher computation efficiency and inversion precision. The CG method is a promising method for full waveform inversion. 
Keywords:
本文献已被 CNKI 等数据库收录!
点击此处可从《煤田地质与勘探》浏览原始摘要信息
点击此处可从《煤田地质与勘探》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