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GFZ Wireless Seismic Array (GFZ-WISE) a Wireless Mesh Network of Seismic Sensors: New Perspectives for Seismic Noise Array Investigations and Site Monitoring

机译:GFZ无线地震阵列(GFZ-WISE)地震传感器的无线网状网络:地震噪声阵列研究和现场监测的新观点

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摘要

Over the last few years, the analysis of seismic noise recorded by two dimensional arrays has been confirmed to be capable of deriving the subsoil shear-wave velocity structure down to several hundred meters depth. In fact, using just a few minutes of seismic noise recordings and combining this with the well known horizontal-to-vertical method, it has also been shown that it is possible to investigate the average one dimensional velocity structure below an array of stations in urban areas with a sufficient resolution to depths that would be prohibitive with active source array surveys, while in addition reducing the number of boreholes required to be drilled for site-effect analysis. However, the high cost of standard seismological instrumentation limits the number of sensors generally available for two-dimensional array measurements (i.e., of the order of 10), limiting the resolution in the estimated shear-wave velocity profiles. Therefore, new themes in site-effect estimation research by two-dimensional arrays involve the development and application of low-cost instrumentation, which potentially allows the performance of dense-array measurements, and the development of dedicated signal-analysis procedures for rapid and robust estimation of shear-wave velocity profiles. In this work, we present novel low-cost wireless instrumentation for dense two-dimensional ambient seismic noise array measurements that allows the real–time analysis of the surface-wavefield and the rapid estimation of the local shear-wave velocity structure for site response studies. We first introduce the general philosophy of the new system, as well as the hardware and software that forms the novel instrument, which we have tested in laboratory and field studies.
机译:在过去的几年中,二维阵列记录的地震噪声分析已被证实能够推导出低至几百米深度的地下土剪切波速度结构。实际上,仅使用几分钟的地震噪声记录,并将其与众所周知的水平-垂直方法相结合,就可以研究出城市中一系列站点下方的平均一维速度结构。具有足够分辨率的深度区域,这对于有源震源阵列勘测是不允许的,同时还减少了进行现场效果分析所需的钻孔数量。然而,标准地震仪器的高成本限制了通常可用于二维阵列测量的传感器的数量(即,数量级为10),从而限制了估计的剪切波速度剖面中的分辨率。因此,二维阵列的场地效应估计研究中的新主题涉及低成本仪器的开发和应用,这可能允许进行密集阵列测量,以及开发专用于信号分析程序以实现快速,强大的功能。估计剪切波速度剖面。在这项工作中,我们提出了用于密集二维环境地震噪声阵列测量的新型低成本无线仪器,该仪器可对表面波场进行实时分析并快速估算局部切波速度结构,以进行场地响应研究。我们首先介绍新系统的一般原理,以及构成新仪器的硬件和软件,我们已经在实验室和现场研究中对其进行了测试。

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