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非均匀网格有限差分法大地电磁测深法正演模拟

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为解决有限差分法大地电磁正演模拟中模拟精度与计算效率之间的矛盾,采用非均匀网格有限差分进行了大地电磁响应计算.基于二维大地电磁方程,推导出非均匀网格剖分下的TM极化模式的大地电磁方程的差分格式.通过均匀半空间模型和低阻异常体模型的正演模拟,验证了非均匀网格差分法的正确性,非均匀网格差分法可以准确反映出复杂模型的大地电磁响应特征,识别异常体分布范围.
Magnetotelluric forward modeling using non-uniform grid finite difference method
In order to solve the contradiction between simulation accuracy and computational efficiency in finite difference magnetotelluric forward modeling,the non-uniform grid finite difference method is used to calculate the magnetotelluric response.Based on the two-dimensional magnetotelluric equation,the difference scheme of TM polarization mode magnetotelluric equation under non-uniform grid subdivision is derived.The correctness of the non-uniform grid difference algorithm is verified by the forward simulation of the uniform half-space model and the low resistance anomaly model.The non-uniform grid difference algorithm can accurately reflect the magnetotelluric response characteristics of the complex model and identify the distribution range of the anomaly body.

magnetotelluric soundingforward modelingfinite difference methodnon-uniform grid

章惠、杜利、魏广仁、隋少强、张慧、刘文辉

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中国石化新星石油公司新能源研究院,北京 100083

华北水利水电大学地球科学与工程学院,河南郑州 450000

大地电磁测深 正演模拟 有限差分法 非均匀网格

中国石油化工集团有限公司科技部项目

JP20011

2024

长江大学学报(自科版)
长江大学

长江大学学报(自科版)

影响因子:0.335
ISSN:1673-1409
年,卷(期):2024.21(4)
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