火炎山土石流現地監測及土石流粒徑分析

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題名:	火炎山土石流現地監測及土石流粒徑分析
作者:	彭楙鈞;Peng, Mao-Chun
貢獻者:	土木工程學系
關鍵詞:	火炎山;土石流;粒徑特性;地聲訊號;Houyenshan;Debris flows;Particle characteristics;Geophone
日期:	2019-08-20
上傳時間:	2019-09-03 12:15:50 (UTC+8)
出版者:	國立中央大學
摘要:	本研究於苗栗三義火炎山一號坑溝內進行土石流事件之現地監測與分析，監測儀器包含雨量計、地聲感應器、縮時攝影機(Time Lapse Camera,TLC)、攝影機(CCD)及無人機(UAV)等。本研究依土石流歷程發展，將一號坑溝的右支流劃分成六個區塊，並在各區段設置縮時攝影機(Time Lapse Camera,TLC)進行監測。三維地聲儀收集土石流所造成的地表震動訊號，再利用快速傅立葉轉換(Fast Fourier Transform, FFT)找出土石流之特徵頻率。2018-2019 年火炎山土石流事件之特徵頻率介於15 至55 赫茲，再利用希爾伯特-黃轉換(Hilbert-Huang Transform,HHT)分析土石流時序-頻率-能量之關係。土石流側積堤及河道上堆積之舌狀堆積顯示較大顆粒的主軸排列有平行河道的趨勢。;The debris flow events in Houyenshan Gullies of Sanyi, Miaoli County were explored in this study by deploying the on-site monitoring system, which includes the rain gauge, geophones, Time Lapse Camers (TLC) , CCD and the unmanned aerial vehicle(UAV). The right tributary of the first gully is delineated into six segments based on the transport process of debris flows, and the movements were captured by the Time Lapse Cameras (TLC) installed in each segment. The ground vibration signals recorded by the three-dimensional geophone were analyzed by the Fast Fourier Transform (FFT). The peak frequency of debris flows at Houyenshan is between 15 and 55 Hz. The frequency modulation process then was analyzed by employing the Hilbert-Huang Transform (HHT). The topography and terrain changes of the debris flow are surveyed by employing both the total station and UAV. The main axis of larger boulders (above the median size) in both the lobes and lateral levees tend to be parallel the flow direction channel.
顯示於類別:	[土木工程研究所] 博碩士論文

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