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首页> 外文期刊>Journal of Applied Geophysics >Detecting lateral inhomogeneity using a 3D Rayleigh wave survey based on numerical simulation and on-site experiment
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Detecting lateral inhomogeneity using a 3D Rayleigh wave survey based on numerical simulation and on-site experiment

机译:使用基于数值模拟和现场实验的3D瑞利波测量检测横向不均匀性

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To deal with the narrow field limitation for the 3D lateral inhomogeneity investigation in the geotechnical engineering, or in urban areas, the paper proposes a radial line survey grid in a cylindrical coordinate system for the Rayleigh wave method. Based upon the cylinder wave features of the wave and the Huygens' principle, the wavefield of the Rayleigh wave recorded by the survey grid can be regarded as a complete 3D wavelleld record excited only by one virtual source at the origin, if the energy attenuation is discarded, and the effects of the multiple sources with the conventional 3D survey grid in a rectangular coordinate system are removed. The numerical method simulates the 3D wavelleld for homogeneous half-space model and lateral inhomogeneity half-space model (represented by a cavity). The wavefronts of the 3D seismic records with the grid for the numerical models are imaged and the 3D dispersion features of the velocity and ellipticity of the Rayleigh wave are analyzed. Following these, an on-site experiment is carried out using the grid for a 3D detection of a sewage well. The results showed that the 3D seismic records in the far-source region acquired by the survey grid, can directly image the wavefront features of the Rayleigh wave and its distortion by the lateral inhomogeneity in a 3D domain. They also show that the anomalies of the 3D velocity and ellipticity dispersion of the local inhomogeneity are similar to that of water waves are scattered by a solid obstacle, which makes it much easier to recognize a cavity compared to that using the complex dispersion anomalies in a 2D profile or the conventional 3D survey grid in a rectangular system. Moreover, the grid can greatly reduce the work-cost of a 3D survey and be adapted well to narrow areas if the excited source is set at the origin of the radial lines. (C) 2020 Elsevier B.V. All rights reserved.
机译:为了处理岩土工程或城市地区的3D横向不均匀性调查的狭窄现场限制,本文提出了一种用于瑞利波方法的圆柱坐标系中的径向线测量网格。基于波浪和霍耶的原理的气缸波特征,通过调查网格记录的瑞利波的波场可以被视为仅在原始的一个虚拟源上兴奋的完整3D波形记录,如果能量衰减是丢弃,并去除在矩形坐标系中与传统的3D测量网格的多个来源的影响被移除。数值方法模拟均匀半空间模型和横向不均匀性半空间模型的3D波形(由腔表示)。对数值模型的网格的3D地震记录的波前进行了成像,分析了瑞利波的速度和椭圆度的3D色散特征。在这些之后,使用电网进行现场实验,用于3D检测污水。结果表明,由测量网格获取的远源区中的3D地震记录,可以通过3D域中的横向不均匀性直接以瑞利波的波前特征及其失真图像。他们还表明,局部不均匀性的3D速度和椭圆性分散的异常类似于水波散射的固体障碍物,这使得与使用复杂的分散异常中的复杂分散异常相比,更容易识别腔在矩形系统中的2D轮廓或传统的3D测量网格。此外,如果激励的源设置在径向线的原点,则该网格可以大大降低3D测量的工作成本,并适应窄区域。 (c)2020 Elsevier B.V.保留所有权利。

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