Citation: | LI Ze-Yang, MA Huan, ZHANG Hao-Nan, DAI Yi-Long, LI Yang, YANG Ying-Yu. 2025. Data Reconstruction of Direct Current Resistivity Method Based on U-Net Convolutional Neural Network. South China Geology, 41(1): 240-248. doi: 10.3969/j.issn.2097-0013.2025.01.020 |
In this paper, a data reconstruction algorithm based on Convolutional Neural Networks (CNN) is proposed for the issue of data mutation caused by humanistic noise in the geophysical resistivity method data acquisition. Given the nonlinear characteristics of the resistivity method control equation, the traditional linear interpolation techniques may lead to a decline in the accuracy of the inversion results. In this study, a CNN model is first constructed and numerical simulation of the resistivity method inversion is carried out by the three-dimensional finite difference method to generate a training dataset and a test dataset. The CNN model is trained using the training set and the U-Net network parameters are optimized based on the loss function results. By comparing the inversion results of data reconstructed with linear interpolation technique and CNN reconstruction of synthetic mutant data, the effectiveness and superiority of CNN in data reconstruction are verified. The results demonstrate that U-Net-CNN can effectively reconstruct nonlinear direct current resistivity method data, providing a new technical approach to improve the accuracy of geophysical data acquisition and the reliability of inversion results.
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U-Net Network Architecture
Example of dataset construction
The loss value of the U-Net model under different hyperparameter configurations
Horizontal stratified medium geoelectric model
Apparent resistivity pseudo-section diagrams of horizontal layered media
Inclined vein-like medium geoelectric model
Apparent Resistivity Pseudo-Section Diagram of Inclined Vein-Like Media
Irregular-shaped medium geoelectric model
Apparent Resistivity Pseudo-Section Diagram of Irregular Media
Comparison of measured reconstructed data apparent resistivity pseudo-section (a, c) and inversion model resistivity section (b, d)