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Distinction of Landslide by Monitoring Acceleration to Autonomous Node In Wireless Sensing Network

机译:通过监测无线传感网络中自治节点的加速度来区别滑坡

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For monitoring natural landslide disaster, wireless sensing node network is so effective system. The sensing node is constructed by some sensors (acceleration, soil moisture, GPS and so on), data processing unit (micro processor) and wireless communication unit. The network topology we have constructed is mesh type. In the system, at sensing landslide, the node will transport the information to host system through the node network by using wireless communication. Generally, in natural field, the landslide is sensed as the changing of acceleration. But, it is so difficult to distinguish the landslide obviously. The acceleration of the sensing node will change by not only the landslide disaster but also collision with several hard blocks like stones. This paper describes the distinction method of landslide disaster by using only the signal of acceleration sensor mounted in the sensing node. The method focuses the time transition of frequency distribution of the acceleration signal. Observing the time transition, the situations of sensing node have been distinguished.
机译:用于监控自然滑坡灾难,无线传感节点网络是如此有效的系统。感测节点由一些传感器(加速度,土壤湿度,GPS等),数据处理单元(微处理器)和无线通信单元构成。我们构建的网络拓扑是网格类型。在系统中,在感测滑坡时,该节点将通过使用无线通信将信息通过节点网络传送到主机系统。通常,在自然场中,被感测滑坡作为加速度的变化。但是,很难明显区分滑坡。传感节点的加速度不仅会改变滑坡灾难,而且还会改变与几块硬块相碰撞。本文仅使用安装在传感节点中的加速度传感器的信号来介绍滑坡灾难的区别方法。该方法将频率分布的时间转换聚焦加速度信号。观察时间转换,传感节点的情况已经区分。

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