Journal of University of Science and Technology of China ›› 2020, Vol. 50 ›› Issue (5): 705-714.DOI: 10.3969/j.issn.0253-2778.2020.05.019

• Original Paper • Previous Articles    

3D time-domain IP forward modeling using unstructured finite element method under uneven terrain

HUANG Du, WU Xiaoping   

  1. 1. Laboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China; 2. National Geophysical Observatory at Mengcheng, Mengcheng 233500, China
  • Received:2019-08-26 Revised:2020-05-08 Accepted:2020-05-08 Online:2020-05-31 Published:2020-05-08

Abstract: It is generally believed that the undulating terrain has little influence on the induced polarization (IP) exploration, because it has no influence under the relatively ideal condition of uniform polarization of the underground medium. However, for the complex medium model with ore body under the condition of undulating terrain, the terrain will certainly have an impact on the induced polarization method. Three have been very few studies on the quantitative characterization of terrain effect on the induced polarization method,mainly because the undulating terrain is not easy to simulate, especially for the three-dimensional model. In this paper, the three-dimensional unstructured finite element numerical simulation of induced polarization is developed. The unstructured mesh is particularly suitable for the numerical simulation of three-dimensional geoelectric model under arbitrary undulating terrain and the study of its influence on induced polarization. With the newly developed method, the three-dimensional induced polarization numerical simulation for plate-shaped and spherical anomaly bodies in rolling terrain is carried out, and the influence of rolling terrain on induced polarization response is discussed. The results show that the asymmetric topography will make the center position of IP anomaly deviate. The larger the slope gradient is, the larger the deviation will be, and the IP amplitude becomes smaller with increasing slope gradient. The asymmetry of polarization anomaly also plays an important role in the topography impact for its IP response.

Key words: induced polarization method, uneven terrain, equivalent resistivity, finite element method, unstructured, 3D forward modeling

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