The Use of Surface Waves in Geotechnical Engineering, which Future?

J. Boaga
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引用次数: 1

Abstract

The use of surface waves (SW) in seismology is well known since the pioneering works after the First World War in the 1920s and 1930s. In the 1950s and 1960s, thanks to computer and instrumental improvements, surface waves started to be intensively adopted in global seismology [1-3]. Engineering applications started shortly after, but for their diffusion we have to wait the work of Stokoe and colleagues which introduced the SASW method (Spectral Analysis of Surface Waves) [4,5]. After the introduction of multi-channels methods, Multi channels Analysis of Surface Waves, SWs rapidly become standard practice in engineering geophysical prospecting. Nowadays surface wave methods are the most powerful and used tools for in situ shear wave velocity estimation, basing on the dispersive properties of the layered media [6-8].
表面波在岩土工程中的应用前景如何?
自第一次世界大战后的20世纪二三十年代的开创性工作以来,表面波(SW)在地震学中的应用已广为人知。在20世纪50年代和60年代,由于计算机和仪器的改进,表面波开始在全球地震学中得到广泛应用[1-3]。工程应用在不久之后就开始了,但为了推广它们,我们必须等待Stokoe及其同事的工作,他们引入了SASW方法(表面波的光谱分析)[4,5]。在引入多通道法、多通道表面波分析等方法后,水波法迅速成为工程地球物理勘探的标准做法。目前,基于层状介质的色散特性,表面波法是最强大和最常用的原位剪切波速估计工具[6-8]。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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