Landslide monitoring system based on water adsorption rate utilizing humidity, accelerometer, and temperature sensors

F. Budiman, E. Susanto, D. Perdana, Husneni Mukhtar, Yulius Anggoro Pamungkas, Yakobus Yulyanto Kevin
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引用次数: 1

Abstract

This study examines the application of a landslide disaster monitoring system based on soil activity information that utilizes humidity, temperature, and accelerometer sensors. An artificial highland was built as the research object, and the landslide process was triggered by supplying the system with continuous artificial rainfall. The soil activities were observed through its slope movement, temperature, and moisture content, utilizing an accelerometer, temperature, and humidity sensors both in dry and wet conditions. The system could well observe the soil activities, and the obtained data could be accessed in real-time and online mode on a website. The time delay in sending the data to the server was 2 seconds. Moreover, the characteristics of soil porosity and its relevance to soil saturation level due to water pressure were studied as well. Kinetic study showed that the water adsorption to soil followed the intraparticle diffusion model with a coefficient of determination R 2 0.99043. The system prototype should be used to build the information center of disaster mitigation, particularly in Indonesia.
基于水分吸附率的滑坡监测系统,利用湿度、加速度计和温度传感器
本研究考察了基于土壤活动信息的滑坡灾害监测系统的应用,该系统利用了湿度、温度和加速度传感器。以人工高地为研究对象,通过向该系统持续提供人工降雨触发滑坡过程。在干燥和潮湿的条件下,利用加速度计、温度和湿度传感器,通过其斜坡运动、温度和水分含量来观察土壤活动。该系统能很好地观测土壤活动,所获得的数据可在网站上实时在线获取。向服务器发送数据的时间延迟为2秒。此外,还研究了水压作用下土壤孔隙度特征及其与土壤饱和水平的关系。动力学研究表明,水对土壤的吸附符合颗粒内扩散模型,决定系数为R 2 0.99043。该系统原型应用于建设减灾信息中心,特别是在印度尼西亚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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