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Joint inversion of Rayleigh-wave dispersion data and vertical electric sounding data: synthetic tests on characteristic sub-surface models

机译:瑞利波频散数据和垂直电测深数据的联合反演:特征地下模型的综合测试

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摘要

In the traditional inversion of the Rayleigh dispersion curve, layer thickness, which is the second most sensitive parameter of modelling the Rayleigh dispersion curve, is usually assumed as correct and is used as fixed a priori information. Because the knowledge of the layer thickness is typically not precise, the use of such a priori information may result in the traditional Rayleigh dispersion curve inversions getting trapped in some local minima and may show results that are far from the real solution. In this study, we try to avoid this issue by using a joint inversion of the Rayleigh dispersion curve data with vertical electric sounding data, where we use the common-layer thickness to couple the two methods. The key idea of the proposed joint inversion scheme is to combine methods in one joint Jacobian matrix and to invert for layer S-wave velocity, resistivity, and layer thickness as an additional parameter, in contrast with a traditional Rayleigh dispersion curve inversion. The proposed joint inversion approach is tested with noise-free and Gaussian noise data on six characteristic, synthetic sub-surface models: a model with a typical dispersion; a low-velocity, half-space model; a model with particularly stiff and soft layers, respectively; and a model reproduced from the stiff and soft layers for different layer-resistivity propagation. In the joint inversion process, the non-linear damped least squares method is used together with the singular value decomposition approach to find a proper damping value for each iteration. The proposed joint inversion scheme tests many damping values, and it chooses the one that best approximates the observed data in the current iteration. The quality of the joint inversion is checked with the relative distance measure. In addition, a sensitivity analysis is performed for the typical dispersive sub-surface model to illustrate the benefits of the proposed joint scheme. The results of synthetic models revealed that the combination of the Rayleigh dispersion curve and vertical electric sounding methods in a joint scheme allows to provide reliable sub-surface models even in complex and challenging situations and without using any a priori information.
机译:在传统的瑞利弥散曲线反演中,通常将层厚度作为建模瑞利弥散曲线的第二个最敏感的参数,并假设其为正确的先验信息。由于层厚度的知识通常不精确,因此使用此类先验信息可能会导致传统的瑞利频散曲线反演陷入某些局部最小值,并且可能会显示与实际解相距甚远的结果。在这项研究中,我们试图通过使用瑞利频散曲线数据与垂直电测深数据的联合反演来避免此问题,在此我们使用公共层厚度将两种方法结合在一起。与传统的瑞利频散曲线反演相比,提出的联合反演方案的关键思想是将方法结合在一个联合雅可比矩阵中,并将层S波速度,电阻率和层厚作为附加参数进行反演。所提出的联合反演方法在六个特征性合成次表面模型上使用无噪声和高斯噪声数据进行了测试:低速半空间模型;分别具有特别硬和软层的模型;从硬层和软层复制的模型用于不同的层电阻率传播。在联合反演过程中,非线性阻尼最小二乘方法与奇异值分解方法一起使用,可以为每次迭代找到合适的阻尼值。拟议的联合反演方案测试了许多阻尼值,并选择了一个最近似当前迭代中观测数据的阻尼值。通过相对距离测量来检查关节反演的质量。此外,对典型的色散次表面模型进行了敏感性分析,以说明所提出的联合方案的好处。综合模型的结果表明,联合方案中瑞利频散曲线和垂直电测深方法的结合,即使在复杂和具有挑战性的情况下,也无需使用任何先验信息即可提供可靠的地下模型。

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