3D crosswell electromagnetic inversion based on radial basis function neural network

被引:0
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作者
Sinan Fang
Zhansong Zhang
Wei Chen
Heping Pan
Jun Peng
机构
[1] Yangtze University,Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education
[2] Yangtze University,College of Geophysics and Petroleum Resources
[3] China University of Geosciences,Institute of Geophysics and Geomatics
[4] Changjiang Institute of Survey Technical Research,undefined
[5] MWR,undefined
来源
Acta Geophysica | 2020年 / 68卷
关键词
crosswell electromagnetic (EM); Three-dimensional (3D) inversion; Radial basis function neural network (RBFNN); Orthogonal least squares (OLS); Improved gram; Schmidt (GS);
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摘要
Crosswell electromagnetic (EM) method has fundamentally improved the horizontal detection ability of well logging and will become an increasingly promising approach for the secondary exploration of hydrocarbon reservoir. We applied orthogonal least squares (OLS) radial basis function neural network (RBFNN) based on improved Gram–Schmidt (G–S) procedure to three-dimensional (3D) crosswell EM inversion problems. In the inversion process of the simplified crosswell model with single-grid conductivity anomalies and normal oil reservoir, compared the inversion results of other five neural networks, OLS-RBFNN was proved to have the best global optimization ability and the fastest sample learning speed and the average inversion error of low conductivity anomalies model (4%) and oil reservoir model (9%) can meet the inversion requirements of crosswell EM method. Only the OLS-RBFNN could achieve ideal inversion results in the most concerned central area of crosswell model, and the inversion accuracy of this algorithm will be more outstanding when the model becomes more complex. Merely using the three-component time-domain crosswell EM data of two wells, the inversion of 3D medium conductivity in the crosswell dominant exploration area can be effectively realized through the nonlinear approximation of the OLS-RBFNN.
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页码:711 / 721
页数:10
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