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Determination of wave velocity for source location of a granite specimen

机译:确定花岗岩样品源位置的波速

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Source location technology has been broadly used for structure monitoring. Source location (damage detection) of the structure is a challenging task due to the complex underground conditions. The basic assumption in many currently available techniques is that the velocity of wave, which is generated by structural damage and propagates in the structure, is considered in the constant value to estimate the source location. If the wave velocity is assumed to be a fixed velocity in the target structure, significant error can occur for detecting the damage location. In this study, laboratory tests were performed to analyze the accuracy of the source location according to the wave velocities. This study proposes a velocity model with the receiver distance, with which we verify the accuracy of the source location. Our results from the proposed velocity model produce an erorr rate of only 4%, which is significantly lower than the error rate of the original source location with a varied velocity. This velocity model achieves a high degree of reliability in damage monitoring.
机译:源定位技术已广泛用于结构监视。由于复杂的地下条件,结构的源位置(损坏检测)是一项艰巨的任务。许多当前可用技术中的基本假设是,将由结构破坏产生并在结构中传播的波速考虑为常数,以估算震源位置。如果假设波速是目标结构中的固定速度,则在检测损坏位置时可能会发生重大错误。在这项研究中,进行了实验室测试,以根据波速分析源位置的准确性。这项研究提出了一个具有接收器距离的速度模型,通过该模型我们可以验证源位置的准确性。我们从提出的速度模型得出的结果产生的误码率仅为4%,这大大低于变化速度下原始源位置的误码率。该速度模型在损坏监控中实现了高度的可靠性。

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