吉林大学学报(地球科学版) ›› 2026, Vol. 56 ›› Issue (2): 673-683.doi: 10.13278/j.cnki.jjuese.20240202

• 地球探测与信息技术 • 上一篇    下一篇

基于超收敛单元片梯度恢复的自适应有限元法音频大地电磁正演

张阳阳1,杜威2   

  1. 1.安徽省勘查技术院,合肥230031

    2.云南大学地球科学学院,昆明650091

  • 出版日期:2026-03-26 发布日期:2026-04-16
  • 基金资助:

    云南省基础研究项目(202301AT070163)


Adaptive Finite Element Method for Audio-Frequency Magnetotelluric Forward Modeling Based on Super Convergent Patch Recovery

Zhang Yangyang1, Du Wei2   

  1. 1. Geological Exploration Technology Institute of Anhui Province, Hefei 230031, China

    2. School of Earth Sciences, Yunnan University, Kunming 650091, China

  • Online:2026-03-26 Published:2026-04-16
  • Supported by:
    Supported by the  Basic Research Project of Yunnan Province (202301AT070163)

摘要: 在音频大地电磁(autio-frequency magnetotelluric, AMT)正演模拟中,常规有限元法(finite element method, FEM)固有地受制于计算精度与效率之间的权衡。为解决这一问题,本文提出了一种基于超收敛单元片梯度恢复(super convergent patch recovery, SPR)的自适应有限元方法。该方法利用后验误差估计动态识别待加密单元,实现鲁棒的局部网格优化;将从SPR计算中求得的高精度梯度直接用于辅助场计算,提升整体正演精度。通过一系列系统性的数值实验,对该算法的精度和计算效率进行了全面验证。在水平层状地层中与常规FEM的精度对比结果表明,本文算法经5次迭代后均方根相对误差仅为1.02%,充分证实了其高精度;在高低阻组合模型的正演计算中,视电阻率随迭代的进行逐步逼近模型的真实电阻率,验证了算法稳健的收敛性;复杂地电模型的数值模拟确证了算法对非均质地质模型的良好适应性。结果表明,基于SPR的后验误差估计方法能够有效识别待加密单元并显著提高辅助场计算精度,实质性地提升了AMT正演模拟的精度。

关键词: 超收敛单元片梯度恢复, 后验误差估计, 自适应有限元法, 音频大地电磁正演

Abstract: In the audio-frequency magnetotelluric (AMT) forward modeling, the conventional finite element method (FEM) is inherently constrained by the trade-off between computational accuracy and efficiency. To address this issue, this study proposes an adaptive finite element method  based on super convergent patch recovery (SPR). This method utilizes a posteriori error estimation to dynamically identify elements that require refinement, enabling robust local mesh optimization, and directly employs the high-accuracy recovered gradient values obtained from the SPR computation for auxiliary field calculation, thereby substantially enhancing the overall forward modeling precision. A series of systematic numerical experiments were conducted to comprehensively validate the algorithm’s accuracy and computational efficiency. First, comparative accuracy results with conventional FEM in horizontally layered media demonstrate that the  root mean square relative error is reduced to just 1.02% after five iterations, fully confirming its high precision. Second, in forward modeling of a composite high- and low-resistivity model, the apparent resistivity values progressively approach the true model resistivity as the iteration proceeds, verifying the algorithm's robust convergence behavior. Finally, simulations of complex geoelectrical structures confirm the algorithm’s strong adaptability to heterogeneous geological models models. The results conclusively show that the SPR-based posteriori error estimation method effectively identifies elements for refinement and significantly improves the accuracy of auxiliary field calculation, thus substantially elevating the accuracy of AMT forward modeling.

Key words: super convergent patch recovery, a posteriori error estimate, adaptive finite element method; , audio-frequency magnetotelluric  , forward modeling

中图分类号: 

  • P631.3
[1] 冯凯, 秦策. 大地电磁(MT)自适应有限元各向异性正演[J]. 吉林大学学报(地球科学版), 2020, 50(6): 1887-1896.
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