期刊文献+

基于电场Helmholtz方程的回线源瞬变电磁法三维正演 被引量:37

Three-dimensional forward calculation for loop source transient electromagnetic method based on electric field Helmholtz equation
下载PDF
导出
摘要 正演是电磁法勘探野外工作参数选取、室内资料处理与解释的基础,精确、稳定、高效的三维正演算法尤为重要.本文采取先求解拉普拉斯域电场、再由Gaver-Stehfest算法获得时间域磁场的思路,基于电场异常场Helmholtz方程实现了交错网格有限差分法和有限体积法对回线源瞬变电磁法的三维正演.通过对比低阻块状体的积分方程法、时域有限差分法、矢量有限单元法和SLDM法的数值解,验证了交错网格有限差分法和有限体积法的正确性.由于交错网格有限差分法、有限体积法和基于矩形块单元的矢量有限单元法将待求电场均定义在矩形块单元棱边上,因此三种数值算法可采用相同方法进行电场待求量编码、计算背景场和后处理.然而,与矢量有限单元法相比,交错网格有限差分法和有限体积法的系数矩阵更加稀疏,求解效率更高.通过对水平低阻板状体三维模型的数值模拟,我们发现本研究中交错网格有限差分法比有限体积法精度更高;再利用一维解析法求解相应三层层状地电模型的感应电动势,我们还发现两种数值算法和一维解析法计算的感应电动势等值线形状吻合程度高,只是数值范围略有差异. Forward and interpretation ; is very important. field firstly, then calculation is the base of parameters selection in field work, data processing, particularly the accurate, stable and efficient three-dimensional forward solver In this paper, based on the strategy that solving the Laplace-domain electrical acquiring the time-domain magnetic field by Gaver-Stehfest algorithm, weemployed staggered finite difference (SFD) and finite volume (FV) to discretize the electrical field Helmholtz equation for three-dimensional forward calculation of loop source transient electromagnetic method. Comparing with the numerical solutions of integral equation (IE), finite difference in time domain (FDTD), vector finite element method (VFEM) and spectral Lanczos decomposition method (SLDM) for low resistivity body in homogeneous half-space, we validated the SFD and FV algorithms. Because the unknown electrical field is arranged on the edge of brick for SFD, FV and VFEM based on brick element, so these three numerical algorithms could utilize the same method for coding the unknown electrical field, computing the background field and post processing. However, comparing with the VFEM, the coefficient matrixes produced by SFD and FV are sparser, so these two algorithms are more efficient. For low resistivity horizontal sheet model, we use SFD, FV and 1D analytical method to compute the induced electromagnetic force (EMF). The results show that SFD has higher accuracy than FV, and the contours of EMF for these three algorithms coincide with each other very well although the range of EMF has fine distinctions.
出处 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2013年第12期4256-4267,共12页 Chinese Journal of Geophysics
基金 国家重点基础研究发展计划(973计划:2013CB733203) 国家地调项目(12120113101800) 中国博士后基金(2012M521498) 中央高校基本科研业务费专项资金联合资助
关键词 HELMHOLTZ方程 回线源 瞬变电磁法 有限差分法 有限体积法 Helmholtz equation, Loop source, Transient electromagnetic method, Finitedifference, Finite volume
  • 相关文献

参考文献37

  • 1Flores C,Peralta Ortega S A. Induced polarization with inloop transient electromagnetic soundings:A case study of mineral discrimination at El Arco porphyry copper,Mexico[J].{H}Journal of Applied Geophysics,2009,(03):423-436.
  • 2Yang D K,Oldenburg D W. Three-dimensional inversion of airborne time-domain electromagnetic data with applications to a porphyry deposit[J].{H}GEOPHYSICS,2012,(02):B23-B34.
  • 3XueGQ,Qin K Z,LiX. Discovery of a Large-scale Porphyry Molybdenum Deposit in Tibet through a Modified TEM Exploration Method[J].{H}JOURNAL OF ENVIRONMENTAL & ENGINEERING GEOPHYSICS,2012,(01):19-25.
  • 4薛国强,陈卫营,周楠楠,李海.接地源瞬变电磁短偏移深部探测技术[J].地球物理学报,2013,56(1):255-261. 被引量:96
  • 5XueG Q,Bai C Y,Yan S. Deep sounding TEM investigation method based on a modified fixed central-loop system[J].{H}Journal of Applied Geophysics,2012.23-32.
  • 6Ezersky M,Legchenko A,Al-Zoubi A. TEM study of the geoelectrical structure and groundwater salinity of the Nahal Hever sinkhole site,Dead Sea shore,Israel[J].{H}Journal of Applied Geophysics,2009,(01):99-112.
  • 7Porsani J L,Bortolozo C A,Almeida E R. TDEM survey in urban environmental for hydrogeological study at USP campus in Sāo Paulo city,Brazil[J].{H}Journal of Applied Geophysics,2012.102-108.
  • 8Porsani J L,Almeida E R,Bortolozo C A. TDEM survey in an area of seismicity induced by water wells in Paraná sedimentary basin,Northern Sāo Paulo State,Brazil[J].{H}Journal of Applied Geophysics,2012.75-83.
  • 9李建慧,朱自强,曾思红,刘树才.瞬变电磁法正演计算进展[J].地球物理学进展,2012,27(4):1393-1400. 被引量:54
  • 10Wang T,Hohmann G W. A finite-difference,time-domain solution for three-dimensional electromagnetic modeling[J].{H}GEOPHYSICS,1993,(06):797-809.

二级参考文献177

共引文献396

同被引文献432

引证文献37

二级引证文献242

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部