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Results and experiences of application of the Refraction Microtremor method for the geophysical investigation ofthe new subway lines in Madrid (Spain)

机译:折射微观测量法在地球物理调查中的应用结果与经验 马德里(西班牙)的新地铁线路

摘要

Geophysical exploration with seismic methods in urban zones presents several disadvantages: the presenceof numerous sources of seismic noise, the scanty penetration when the seismic source is a hammer andthe disability to detect buried low-velocity beds. Recently (Louie, 2001) a new method of seismicinvestigation has been developed, which allows vertical modeling of Raleygh waves from spectral analysis(Vphase/frequency) using the seismic signal registered with conventional seismographs and geophones.This method allows to detect low-velocity buried beds of great interest in tunneling, and to reachdepths below 50 meters. In this work we discuss the conditions of application and experiences obtainedduring the 2005 geophysical surveys carried out in Madrid before the excavation of the new subwaytunnels
机译:在城市地区采用地震方法进行地球物理勘探存在几个缺点:存在大量地震噪声源,当地震源为锤子时穿透力不足,并且无法探测低速埋藏的地层。最近(Louie,2001)开发了一种新的地震调查方法,该方法可以使用常规地震仪和地震检波器记录的地震信号通过频谱分析(Vphase / frequency)对Raleygh波进行垂直建模,该方法可以检测低速掩埋对隧道技术非常感兴趣,并能到达50米以下的深度。在这项工作中,我们讨论了在开挖新的地铁隧道之前在马德里进行的2005年地球物理调查期间的应用条件和经验。

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