THE THREE-DIMENSIONAL IMAGING TECHNOLOGY AND ITS IMPROVEMENT FOR GEOLOGICAL STRUCTURE BASED ON TRT SYSTEM

BAI Ming-Zhou, TIAN Gang, WANG Cheng-Liang, SHI Hai, NIE Yi-Cong, SHEN Yu-Peng
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引用次数: 2

Abstract

The TRT technology is used to achieve recognition of the disaster body with the help of seismic wave reflection principle; it can locate disaster body using a confocal ellipsoid changing with time composed by seismic focus and the receiving focus. By comparing the abnormal image area formed by TRT technology with the tunnel disaster area caused by the earthquake, the TRT anomaly area is divided into four types, which is cluster abnormal area, single abnormal area, faulted abnormal area and interbedded abnormal area. Aiming at TRT technology's own problems which is that the calculation of direct wave velocity is not enough accurate and the setting of background wave velocity is unreasonable, a corresponding improvement method is proposed. On one hand, to get the actual direct wave velocity between seismic focus and the receiving focus, through calculating the minimum actual spreading track of the direct wave in the tunnel. On the other hand, to obtain 1-a confidence interval of actual direct wave velocity in the condition of Gaussian distribution, based on the distribution of direct wave velocity. To entry the upper and lower limits of the confidence interval as the background velocity into the TRT system, and gain two sets TRT's image, which gets rid of the singleness and blindness in setting the background wave velocity, and makes a certain confidence interval consideration for the improved geological hazard forecasting. The result of the present example shows that the effect of improved geological hazard forecasting is much better than the forecasting effect of setting the background wave velocity, in a certain degree, that avoids the possibility of omission in disaster prediction.

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基于TRT系统的地质构造三维成像技术及其改进
利用地震波反射原理,利用TRT技术实现对灾体的识别;利用地震焦点与接收焦点组成的随时间变化的共聚焦椭球体来定位灾体。通过将TRT技术形成的异常图像区与地震引起的隧道灾区进行对比,将TRT异常区划分为集群异常区、单一异常区、断裂异常区和互层异常区四种类型。针对TRT技术自身存在的直波速计算不够精确、背景波速设置不合理等问题,提出了相应的改进方法。一方面,通过计算隧道内最小实际传播路径,得到地震震源与接收震源之间的实际直波速;另一方面,根据直波速的分布,得到高斯分布条件下实际直波速的1-a置信区间。将置信区间的上下限作为背景波速输入到TRT系统中,得到两组TRT图像,消除了背景波速设置的单一性和盲目性,为改进的地质灾害预测提供了一定的置信区间考虑。算例结果表明,改进后的地质灾害预测效果远好于设置背景波速的预测效果,在一定程度上避免了灾害预测遗漏的可能。
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