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浅水区海浪电磁噪声对大地电磁阻抗估计的影响
引用本文:潘林冬, 李予国, 葛佳琦, 吴云具. 2023. 浅水区海浪电磁噪声对大地电磁阻抗估计的影响. 地球物理学报, 66(11): 4742-4752, doi: 10.6038/cjg2022Q0228
作者姓名:潘林冬  李予国  葛佳琦  吴云具
作者单位:1. 中国海洋大学海洋地球科学学院, 山东青岛 266100; 2. 海底科学与探测技术教育部重点实验室, 山东青岛 266100
基金项目:国家自然科学基金项目(91958210), 国家重点研发计划项目(2019YFC1408100)资助
摘    要:在浅水区海洋大地电磁(MT)勘探中, 海浪运动频带范围内(约0.05~0.8 Hz)阻抗估计结果欠佳, 这一直是困扰地球物理工作者的难题.本文基于三层海洋地电模型推导了二维和三维海浪运动感应电磁场(简称海浪感应电磁场)表达式, 分析了海浪感应电磁场的平面波传播特性.借鉴MT场趋肤深度和阻抗的概念, 推导出海浪感应电磁场的趋肤深度和阻抗表达式, 分析了浅水区海浪感应电磁场和MT场趋肤深度和阻抗的差异.在海底介质中, 海浪感应电磁场的衰减速度要比MT场衰减速度大约快2个量级, 因而它无法用于探测海底深部电性结构.海浪感应电磁场阻抗幅值比MT阻抗幅值小2~3个量级.海浪感应电噪声强度约为大地电场强度的10%, 而海浪感应磁噪声比地球变化磁场大1~2个量级, 故海浪感应电噪声对大地电场的影响较小, 但海浪感应磁噪声对地球变化磁场的影响较大.海浪感应电磁阻抗相位在-90°(TE模式)和90°(TM模式)附近, 偏差小于0.06°, 而均匀半空间介质MT阻抗相位为-45°(TE模式)和135°(TM模式).通过引入"复合阻抗"概念, 探讨了海浪感应电磁场对海洋MT阻抗估计结果的影响.

关 键 词:浅水区   海浪感应电磁场   MT场   趋肤深度   复合阻抗
收稿时间:2022-04-05
修稿时间:2023-06-25

Impacts of electromagnetic noise of shallow water ocean waves on magnetotelluric impedance estimation
PAN LinDong, LI YuGuo, GE JiaQi, WU YunJu. 2023. Impacts of electromagnetic noise of shallow water ocean waves on magnetotelluric impedance estimation. Chinese Journal of Geophysics (in Chinese), 66(11): 4742-4752, doi: 10.6038/cjg2022Q0228
Authors:PAN LinDong  LI YuGuo  GE JiaQi  WU YunJu
Affiliation:1. College of Marine Geosciences, Ocean University of China, Qingdao Shandong 266100, China; 2. Key Lab of Submarine Geosciences and Prospecting Technique of Ministry of Education, Qingdao Shandong 266100, China
Abstract:In shallow water marine magnetotelluric (MT) exploration, the impedance estimation within the wave motion frequency band (about 0.05~0.8 Hz) is poor. Based on the three-layer ocean geoelectric model, the expressions of ocean waves induced electromagnetic (OWEM) fields are derived. And the propagation characteristics of OWEM fields are analyzed. The expressions of the skin depth and impedance expressions of OWEM fields are derived, and the differences between the skin depth and impedance of OWEM and MT fields in shallow water areas are analyzed. In the seabed medium, the attenuation rate of the OWEM field is about two orders of magnitude faster than that of the MT field, so it cannot be used to detect deep electrical structure. The amplitude of OWEM impedance is 2~3 orders of magnitude smaller than that of MT impedance. The intensity of the wave-induced electric noise is about 10% of that of the telluric field, and the wave-induced magnetic noise is 1~2 orders of magnitude larger than the varying magnetic field of the Earth, so the wave-induced electric noise has little impact on the telluric field, but the wave-induced magnetic noise has a great impact on the Earth's varying magnetic field. The phase of OWEM impedance is around -90° (TE mode) and 90° (TM mode), the deviation is less than 0.06°, while the MT impedance phase in homogeneous half-space is -45° (TE mode) and 135° (TM mode). By introducing the concept of "composite impedance", the influence of OWEM fields on marine MT impedance estimation is discussed.
Keywords:Shallow water  Ocean waves induced electromagnetic (OWEM) fields  Magnetotelluric (MT) fields  Skin depth  Composite impedance
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