Mutually Constrained Inversion of Common Offset GPR Reflection and Surface Wave Dispersion Data in Layered Media

Shufan Hu, Yonghui Zhao, S. Ge
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Abstract

Summary Ground penetrating radar (GPR) and seismic surface wave methods (SWMs) are widely used in near-surface surveys. For the most frequently used common offset GPR reflection data, a key requirement for proper imaging of subsurface reflectors is an accurate velocity model, especially when dipping layers are present in the subsurface. For the inversion of surface wave data in a layered system, the model parameterization is critical if a priori information is not available. Here, we presented a possible way for mutually constrained inversion of the common offset GPR reflection traveltime and surface wave dispersion data. We used the depth of interfaces to link the model parameters of GPR and the surface wave method based on structural similarity. The parameterization problem of the surface wave data inversion is mitigated by using interface constraints from GPR profile, we then inverted the layered model parameters including thickness and velocities of EM wave and shear wave simultaneously by using the alternate coupling strategy. Test on a synthetic example showed that the estimation of depth and EM velocity in GPR result is significantly improved, while, the simultaneous use of both datasets could provide a reliable parametrization for the surface wave inversion.
层状介质中共偏移GPR反射与面波色散数据的相互约束反演
探地雷达(GPR)和地震表面波法(SWMs)在近地面测量中得到了广泛的应用。对于最常用的通用偏置GPR反射数据,对地下反射器进行正确成像的关键要求是精确的速度模型,特别是当地下存在倾斜层时。对于层状系统表面波数据的反演,如果没有先验信息,模型参数化是至关重要的。在这里,我们提出了一种共同偏移GPR反射走时和表面波色散数据相互约束反演的可能方法。基于结构相似性,利用界面深度将探地雷达模型参数与面波法模型参数联系起来。利用探地雷达剖面的界面约束,解决了面波数据反演的参数化问题,并采用交替耦合策略同时反演了电磁波和横波的厚度和速度等层状模型参数。综合算例测试表明,探地雷达结果中深度和电磁速度的估计有了明显改善,同时使用两种数据集可以为表面波反演提供可靠的参数化。
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