| 基于COMSOL的起伏地形三维大地电磁数值模拟北大核心CSCD |
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| 引用本文： | 李忠乾,李长伟,宋卫文,周翔,伍师莹,熊彬.基于COMSOL的起伏地形三维大地电磁数值模拟北大核心CSCD[J].地质与勘探,2022,58(1):107-117. |
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| 作者姓名： | 李忠乾 李长伟 宋卫文 周翔 伍师莹 熊彬 |
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| 作者单位： | 桂林理工大学地球科学学院,广西桂林 541006;桂林理工大学地球科学学院,广西桂林 541006;广西隐伏金属矿产勘查重点实验室,广西桂林 541006 |
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| 基金项目： | 国家自然科学基金（编号：41464002,42174080）;广西自然科学基金(编号:2020GXNSFAA297079);
广西自然科学基金创新研究团队（编号：GXNSFGA380004）,广西隐伏金属矿产勘查重点实验室系统研究课题（编号：12-B-03,14-A-01-05）;桂林理工大学博士科研启动资金（编号：GUTQDJJ2011038）资助 |
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| 摘 要： | COMSOL是一个多物理场仿真软件,笔者尝试将其应用于大地电磁法的数值模拟,研究起伏地形对大地电磁响应的影响及解决方案。本文由麦克斯韦方程组出发,施加第一类边界条件,将地形起伏数字化为参数化曲面,导入COMSOL进行计算。在对COMSOL的精度进行了验证的基础上,分析不同频点所需内存以及自由度,然后选择合适的频点进行研究。将三维起伏地形的模拟结果与无地形起伏时的结果进行对比,总结出山谷、山峰地形对三维大地电磁响应的影响,发现在XY模式下,地形对视电阻率的影响大于相位,在视电阻率等值线图中能够清晰地看出起伏地形的轮廓,而在YX模式下,地形对相位的影响大于对视电阻率的影响。最后,利用“比值法”进行地形校正,校正前由于起伏地形影响,在异常体附近会出现部分视电阻率数值跳跃现象,通过校正有效抑制了起伏地形对异常体附近视电阻率的影响,校正后的视电阻率曲线整体上移,并且异常体周围的视电阻率值也趋于背景场值,获得了较好的效果。
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| 关 键 词： | COMSOL 大地电磁 三维起伏地形 地形校正 数值模拟 |
| 收稿时间： | 2021/4/26 0:00:00 |
| 修稿时间： | 2021/10/28 0:00:00 |
3D magnetotelluric modeling with undulating terrain based on COMSOL |
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| LI Zhongqian,LI Changwei,SONG Weiwen,ZHOU Xiang,WU Shiying,XIONG Bin.3D magnetotelluric modeling with undulating terrain based on COMSOL[J].Geology and Prospecting,2022,58(1):107-117. |
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| Authors: | LI Zhongqian LI Changwei SONG Weiwen ZHOU Xiang WU Shiying XIONG Bin |
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| Institution: | School of Earth Sciences, Guilin University of technology, Guilin, Guangxi; Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin , Guangxi |
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| Abstract: | COMSOL is a multi-physical field simulation software. We try to apply it to the numerical simulation of the magnetotelluric (MT) method to study the influence of undulating terrain on MT response and its solution. Based on Maxwell''s equations, the first kind of boundary conditions are applied to the model and the topographic relief is digitized into a parameterized surface, which is imported into COMSOL for calculation. On the basis of verifying the accuracy of COMSOL, the required memory and degrees of freedom for different frequency points are analyzed, and then the appropriate frequency points are selected for research. We compare three-dimensional undulating terrain simulation results with that no terrain relief, and examine the influence of the valley and the mountain terrain on three-dimensional MT response. Research suggests that in the XY mode, the influence of terrain is greater than that of the phase of resistivity, the apparent resistivity in the contour map can clearly show the outline of undulating terrain; while under the mode of YX, topography has more effect on phase than on apparent resistivity. Finally, using the "ratio method" to make topographic correction to remove the jump of some apparent resistivity values near the abnormal body due to original terrain. Through such correction, the influence of undulating terrain on apparent resistivity near the abnormal body is effectively restrained. After the correction, the apparent resistivity curve is shifted overall upward, and the apparent resistivity values around the abnormal body tend to be the background field, meaning good results obtained. |
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| Keywords: | COMSOL magnetotelluric undulating terrain topographic correction numerical modeling |
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