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S-wave velocity profiling from refraction microtremor Rayleigh wave dispersion curves via PSO inversion algorithm

机译:通过PSO反转算法从折射微调瑞利波色散曲线的S波速度分析

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The refraction microtremor method has been increasingly used as an appealing tool for investigating near surface S-wave structure. However, inversion, as a main stage in processing refraction microtremor data, is challenging for most local search methods due to its high nonlinearity. With the development of data optimization approaches, fast and easier techniques can be employed for processing geophysical data. Recently, particle swarm optimization algorithm has been used in many fields of studies. Use of particle swarm optimization in geophysical inverse problems is a relatively recent development which offers many advantages in dealing with the nonlinearity inherent in such applications. In this study, the reliability and efficiency of particle swarm optimization algorithm in the inversion of refraction microtremor data were investigated. A new framework was also proposed for the inversion of refraction microtremor Rayleigh wave dispersion curves. First, particle swarm optimization code in MATLAB was developed; then, in order to evaluate the efficiency and stability of proposed algorithm, two noise-free and two noise-corrupted synthetic datasets were inverted. Finally, particle swarm optimization inversion algorithm in refraction microtremor data was applied for geotechnical assessment in a case study in the area in city of Tabriz in northwest of Iran. The S-wave structure in the study area successfully delineated. Then, for evaluation, the estimated Vs profile was compared with downhole data available around of the considered area. It could be concluded that particle swarmoptimization inversion algorithm is a suitable technique for inverting microtremor waves.
机译:折射微调法越来越多地用作研究近表面S波结构的吸引力工具。然而,作为处理折射微调数据中的主要阶段的反转是由于其高的非线性而充满了大多数本地搜索方法的具有挑战性。随着数据优化方法的发展,可以采用快速和更简单的技术来处理地球物理数据。最近,粒子群优化算法已在许多研究领域中使用。在地球物理逆问题中使用粒子群优化是一个相对近期的发展,在处理这些应用中固有的非线性方面提供了许多优势。在该研究中,研究了粒子群优化算法在折射微良数据反转中的可靠性和效率。还提出了一种新的框架,用于折射微调瑞利波分散曲线的反转。首先,开发了MATLAB中的粒子群优化代码;然后,为了评估所提出的算法的效率和稳定性,反转了两个无噪声和两个噪声损坏的合成数据集。最后,在伊朗西北地区塔德里兹市地区的岩土评估中,应用了折射微调数据中的粒子群优化反演算法。研究区中的S波结构成功划定。然后,为了评估,将估计的VS配置文件与所考虑的区域的井下数据进行比较。可以得出结论,粒子群化反演算法是用于反转微反射波的合适技术。

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