使用COMSOL多物理学的地面短暂电磁数据的高斯-牛顿逆转
1College of Geology and Environment, Xi'an University of Science and Technology, Xi'an, 710054, Shaanxi, China. lifan@xust.edu.cn.
Scientific reports
|December 1, 2025
概括
本研究介绍了使用COMSOL多物理学的过渡电磁 (TEM) 数据的高斯-牛顿逆转框架. 该方法准确地建模了地下结构,在资源勘探的现场应用中被证明是有效的.
科学领域:
- 地质物理学 地质物理学
- 计算电磁学 计算机电磁学
背景情况:
- 过渡电磁 (TEM) 方法对于地下勘探至关重要.
- 科姆索尔多物理提供灵活的3D建模,但在灵敏度矩阵计算反转方面面临挑战.
研究的目的:
- 开发一个强大的高斯-牛顿逆转框架用于使用COMSOL多物理的TEM数据.
- 为了克服灵敏度矩阵计算在3D TEM反转中的计算挑战.
主要方法:
- 在COMSOL中实现了一个虚拟磁源和辅助场方法,用于3D灵敏度矩阵计算.
- 将灵敏度矩阵计算与高斯-牛顿算法集成为代反转工作流.
主要成果:
- 与分析解决方案相比,在前建模中实现了高精度 (相对误差<1.4%).
- 在一个复杂的分层模型中,仅在4次代中证明了强大的融合.
- 在现场案例研究中,成功地划出了导水区,与钻井数据一致.
结论:
- 开发的框架为3D TEM逆转提供了方便和准确的计算解决方案.
- 该方法显著提高了TEM在复杂的地质场景中的实际适用性.
- 通过数值模拟和在煤矿环境中的现场案例研究来验证.
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