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IMU Based Real Time Underground Soil Movement Detection System: An Illustrative Investigation

机译:基于IMU的实时地下土壤运动检测系统的说明性研究

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Real-time landslide hazard threat assessments (LHTAs) are vital, as landslides in mountainous regions are the costliest and deadliest natural disasters. Landslides are significantly difficult to predict, due to the high variability of slope stability in relation to both space and time. Intrinsic factors (i.e. topography, geology, soil condition, engineering properties, etc.) and extrinsic factors (i.e. rainfall, land cover, earthquakes, volcanoes, etc.) influence the slope stability and landslide triggering. To date, precipitation estimation, high-resolution imagery, and elevation maps enable the threat of rainfall-triggered landslides to be predicted. It is vital to assess soil `movement distance' and `velocity', as the potential for a landslide depends on the non-uniform nature of the structural forces that hold a slope together and on the physical mechanisms that trigger the landslide. This manuscript demonstrates the development of a sensor network that enables LHTAs by detecting landslides' related `movement distance' and `velocity' in real time. The sensor network consists of underground sensors (i.e. an accelerometer, a gyroscope and a magnetometer) that enable the movements of the bottom soil layers to be detected. The aim is to capture the soil `movement distance' and `velocity' in a landslide, using acceleration and relative angular movement data, via the concept used in an inertial measurement unit (IMU).
机译:实时滑坡灾害威胁评估(LHTA)至关重要,因为山区的滑坡是最昂贵,最致命的自然灾害。由于边坡稳定性随时间和空间的高度变化,滑坡很难预测。内在因素(即地形,地质,土壤条件,工程特性等)和外在因素(即降雨,土地覆盖,地震,火山等)影响边坡稳定性和滑坡触发。迄今为止,降水估计,高分辨率图像和高程图可以预测降雨触发的滑坡的威胁。评估土壤的“运动距离”和“速度”至关重要,因为滑坡的可能性取决于将斜坡保持在一起的结构力的非均匀性质以及引发滑坡的物理机制。该手稿演示了通过实时检测滑坡相关的“运动距离”和“速度”来实现LHTA的传感器网络的发展。传感器网络由地下传感器(例如,加速度计,陀螺仪和磁力计)组成,这些传感器可以检测底部土壤层的运动。目的是通过惯性测量单元(IMU)中使用的概念,利用加速度和相对角运动数据来捕获滑坡中的土壤“运动距离”和“速度”。

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