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首页> 外文期刊>Journal of Applied Geophysics >Multimodal inversion of guided waves in georadar data
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Multimodal inversion of guided waves in georadar data

机译:雷达数据中导波的多模态反演

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We analyze the dispersive characteristics of the electromagnetic guided waves (at georadar frequency) to infer the electrical properties of materials that constitute a layered wave guide.WARR (Wide Angle Reflection and Refraction) georadar acquisitions could be carried out in TE (Transverse Electric) configuration to collect the full wavefield at different offset from the source. The dispersive curves of TE modes are obtained by transforming the space-time acquisition into frequency-wavenumber domain (f-k spectrum); the relative maxima in the f-k spectrum for each frequency represent the different propagation modes.We adopt both global and local inversion algorithms for minimizing the misfit function between computed and theoretical curves in order to obtain a 1D model of the layered subsoil (thicknesses and electrical permittivity). We perform a multimodal and multilayer inversion of the dispersive events.The results of two field cases will be discussed; the first one refers to the propagation in a confined waveguide (layered subsoil) and the other in a leaky waveguide (snow cover on a glacier).
机译:我们分析了电磁导波的色散特性(在地雷达频率下),以推断构成分层波导的材料的电性能.WARR(广角反射和折射)地雷达可以在TE(横向电)配置中进行采集收集与波源不同偏移的整个波场。通过将时空采集转换为频率-波数域(f-k频谱),可获得TE模式的色散曲线。 fk频谱中每个频率的相对最大值表示不同的传播模式。我们采用全局和局部反演算法来最小化计算曲线和理论曲线之间的失配函数,以便获得层状地下土壤的一维模型(厚度和介电常数) )。我们对色散事件进行多模态和多层反演。将讨论两种现场情况的结果;第一个是在密闭波导(分层的地下土壤)中传播,另一个是在泄漏波导(冰川上的雪盖)中传播。

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