journal article·2020-08-01Open access

Comparative study of 3D joint inversion based on multi-section resistivity data

Yuanchao Ou, Pingsong Zhang, Chang Liu, Lei Tan, Binyang Sun

AIP Advances· Volume 10· Issue 8

Abstract

A 3D joint inversion of 2D electrical prospecting data can effectively solve the shortcomings of the 2D electrical method in detecting the spatial forms of anomalous bodies. However, the direction and interval between 2D electrical prospecting survey lines can affect the workload of field prospectors and the accuracy of the subsequent 3D inversion. This study established a physical model of an indoor water tank. Multiple sections of 2D electrical survey lines were laid and survey line data was acquired. The intersection angles between 2D electrical survey lines and anomalous bodies as well as the relations between the 3D inversion characteristics and 2D electrical prospecting data for different line intervals were studied. The results of this study indicate that the electrical response of cylindrical anomalous bodies tends to become weaker, first slowly and then faster, with a decrease in the angle. When the intersection angle is between 60° and 90°, the inverted forms of the anomalous bodies are unchanged. When the interaction angle is less than 60°, there is a significant twisting of the bodies and the electrical response is obviously weaker. The 3D joint inversion imaging using multi-section resistivity data can effectively improve the recognition on the spatial forms of objects. However, the joint inversion obtained with different survey line intervals varies in how precisely the objects are depicted. The increase in the interval between survey lines can be divided into four main stages in terms of the 3D joint inversion. To maintain the efficiency of practical prospecting and because survey data forming shallow strata are affected by external interference, it was found experimentally that the optimum interval for the effective depiction of the locations and forms of objects ranges from 8 cm to 12 cm. Specifically, the least number of 2D survey lines can be deployed while ensuring the overall accuracy and reliability of the survey result when the survey line interval/2D electrical prospecting inversion depth ranges from 8/17 to 12/17. The study results may help us to guide the arrangement of electrical survey lines in field prospecting and improve construction efficiency and the accuracy of joint inversion.
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Research context

OpenAlex topics: Geophysical and Geoelectrical Methods · Geophysical Methods and Applications · Seismic Waves and Analysis

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

Affiliations

State Key Laboratory of Mining Response and Disaster Prevention and Control in Deep Coal Mines, Anhui University of Science and Technology 1 , Huainan 232001, China

School of Earth and Environment, Anhui University of Science and Technology 2 , Huainan 232001, China

Zhejiang Guangchuan Engineering Consulting Co., Ltd. 3 , Hangzhou 310020, China

Funding

National Natural Science Foundation of China · Key R&D Program Projects in Anhui Province · Graduate Innovation Found Project of Anhui University of Science and Technology

References (24)

Show source-provided references
1. A comparison of the Gauss−Newton and quasi-Newton methods in resistivity imaging inversion10.1016/s0926-9851(01)00106-9 ↗
2. Properties and effects of measurement errors on 2D resistivity imaging surveying10.3997/1873-0604.2003001 ↗
3. A comparison of smooth and blocky inversion methods in 2D electrical imaging surveys10.1071/eg03182 ↗
4. Two-dimensional direct current (DC) resistivity inversion: Data space Occam’s approach10.1016/j.pepi.2008.06.022 ↗
5. Study on 3D resistivity inversion using conjugate gradient method10.1002/cjg2.55 ↗
6. Geoelectric method for investigating saltwater intrusion into fresh aquifer in Deghele community of Warri South Local Govt. Area of Delta State, Nigeria
7. Three-dimensional parallel electric surveying and its applications in water disaster exploration in coal mines
8. Mapping desiccation fissures using 3-D electrical resistivity tomography10.1016/j.jappgeo.2012.06.002 ↗
9. 3D electrical resistivity inversion with least-squares method based on inequality constraint and its computation efficiency optimization10.6038/j.issn.0001-5733.2012.01.025 ↗
10. 3D resistivity inversion incorporating topography based on unstructured meshes10.6038/cjg20150808 ↗
11. Multi-electrode 3D resistivity imaging of alfalfa root zone10.1016/j.eja.2009.08.005 ↗
12. Contrast between 2D inversion and 3D inversion based on 2D high-density resistivity data10.1016/s1003-6326(14)63051-x ↗
13. Aquifer characterization based on geoelectric survey data in Issele Uku, Delta State, Nigeria10.1063/1.5094583 ↗
14. 3D joint inversion of goaf with geological information
15. Study on the evolution rule of land damage based on electrical resistivity imaging technology in mining face10.1007/s10706-019-00905-1 ↗
16. 3-D inversion of high density resistivity method based on 2-D exploration data and its application
17. 3-D processing technology of high density resistivity data and application to urban ground investigation
18. 3D resistivity inversion using 2D measurements of the electric field10.1046/j.1365-2478.2001.00241.x ↗
19. 3-D inversion of high density resistivity method based on 2-D high-density electrical prospecting data and its engineering application
20. Equation estimation of porosity and hydraulic conductivity of Ruhrtal aquifer in Germany using near surface geophysics10.1016/j.jappgeo.2012.06.001 ↗
21. Unstructured grid based 2-D inversion of VLF data for models including topography10.1016/j.jappgeo.2011.07.011 ↗
22. Application of three-dimensional high density resistivity technique in detecting roof water
23. Effectiveness of electrical resistivity method in coastal hydrogeophysical studies
24. Collecting method and system for distributive parallel intelligent electrode potential difference signals