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Systems and Sensors for Debris-flow Monitoring and Warning

机译:泥石流监测和预警系统和传感器

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Debris flows are a type of mass movement that occurs in mountain torrents. They consist of a high concentration of solid material in water that flows as a wave with a steep front. Debris flows can be considered a phenomenon intermediate between landslides and water floods. They are amongst the most hazardous natural processes in mountainous regions and may occur under different climatic conditions. Their destructiveness is due to different factors: their capability of transporting and depositing huge amounts of solid materials, which may also reach large sizes (boulders of several cubic meters are commonly transported by debris flows), their steep fronts, which may reach several meters of height and also their high velocities. The implementation of both structural and non-structural control measures is often required when debris flows endanger routes, urban areas and other infrastructures. Sensor networks for debris-flow monitoring and warning play an important role amongst non-structural measures intended to reduce debris-flow risk. In particular, debris flow warning systems can be subdivided into two main classes: advance warning and event warning systems. These two classes employ different types of sensors. Advance warning systems are based on monitoring causative hydrometeorological processes (typically rainfall) and aim to issue a warning before a possible debris flow is triggered. Event warning systems are based on detecting debris flows when these processes are in progress. They have a much smaller lead time than advance warning ones but are also less prone to false alarms. Advance warning for debris flows employs sensors and techniques typical of meteorology and hydrology, including measuring rainfall by means of rain gauges and weather radar and monitoring water discharge in headwater streams. Event warning systems use different types of sensors, encompassing ultrasonic or radar gauges, ground vibration sensors, videocameras, avalanche pendulums, photocells, trip wires etc. Event warning systems for debris flows have a strong linkage with debris-flow monitoring that is carried out for research purposes: the same sensors are often used for both monitoring and warning, although warning systems have higher requirements of robustness than monitoring systems. The paper presents a description of the sensors employed for debris-flow monitoring and event warning systems, with attention given to advantages and drawbacks of different types of sensors.
机译:泥石流是山区洪流中发生的一种群众运动。它们由水中的高浓度固体物质组成,并以陡峭的波浪形流动。泥石流可以被认为是介于滑坡和洪水之间的一种现象。它们是山区最危险的自然过程之一,可能在不同的气候条件下发生。它们的破坏性是由于不同的因素造成的:它们具有运输和沉积大量固体物质的能力,固体物质也可能达到大尺寸(通常由碎屑流运送几立方米的巨石),其陡峭的锋面可能达到几米。高度以及它们的高速当泥石流危及路线,市区和其他基础设施时,往往需要同时执行结构性和非结构性控制措施。在旨在减少泥石流风险的非结构性措施中,用于泥石流监测和预警的传感器网络起着重要作用。特别是,泥石流预警系统可以分为两大类:预先预警和事件预警系统。这两类使用不同类型的传感器。预警系统基于监测致病性水文气象过程(通常是降雨),旨在在触发可能的泥石流之前发出预警。事件警报系统基于在这些过程进行时检测碎片流。与提前警告的交货时间相比,它们的交货时间要短得多,但也不太容易发生误报警。泥石流预警是采用气象和水文学特有的传感器和技术,包括通过雨量计和天气雷达测量降雨并监测源头水流中的水排放。事件预警系统使用不同类型的传感器,包括超声波或雷达仪表,地面振动传感器,摄像机,雪崩摆,光电管,跳闸线等。泥石流的事件预警系统与泥石流监控功能紧密相关。研究目的:尽管警告系统比监视系统对鲁棒性的要求更高,但监视和警告通常都使用相同的传感器。本文介绍了泥石流监测和事件预警系统中使用的传感器,并着重介绍了不同类型传感器的优缺点。

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