反演(地质)
时域有限差分法
算法
计算机科学
合成数据
编码(集合论)
有限差分
有限体积法
时域
有限差分法
地球物理学
地质学
数学分析
数学
物理
机械
光学
集合(抽象数据类型)
地震学
构造学
程序设计语言
计算机视觉
作者
T. Støren,J. J. Zach,Frank A. Maaø
出处
期刊:70th EAGE Conference and Exhibition incorporating SPE EUROPEC 2008
日期:2008-06-09
被引量:21
标识
DOI:10.3997/2214-4609.20147963
摘要
Gradient-based 3D inversion of controlled-source electromagnetic (CSEM) data requires the gradient to a data-misfit functional to be computed within the volume where we seek to find a resistivity model that explains the observed data. Since 3D inversion typically requires more than 100 iterations in order to converge to a good model, fast modelling is important to make 3D inversion a feasible tool in advanced interpretation of CSEM data. We have previously presented a fast finite-difference time-domain (FDTD) modeling code which reduces the computational time of a typical modelling scenario by a factor of 40. In this presentation we show how we use this FDTD modeling to efficiently compute the misfit gradient. A benefit of this approach is that the gradient can be computed for several frequencies in one forward modelling thus saving valuable computational resources when inverting data from a large number of receivers. We present results showing that the gradients obtained are well-behaved. We also present results from inversion of synthetic data based on these gradient calculations showing that, for this specific example, a good result was obtained for the inverted resistivity model after relatively few iterations.
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