Model tests and analysis on development process of debris flow
碩士 === 國立暨南國際大學 === 地震與防災工程研究所 === 94 === Experiments on the development of debris flow using flume and slope model tests are performed to investigate the following two factors:(1) The density of soil and (2) Rainfall intensity. Feasibility of using the method of superposition to calculate the disch...
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ndltd-TW-094NCNU01400022016-06-01T04:14:21Z http://ndltd.ncl.edu.tw/handle/42103570850700513335 Model tests and analysis on development process of debris flow 探討土石流發生過程之模型試驗與分析 Li-Kang Hu 胡立康 碩士 國立暨南國際大學 地震與防災工程研究所 94 Experiments on the development of debris flow using flume and slope model tests are performed to investigate the following two factors:(1) The density of soil and (2) Rainfall intensity. Feasibility of using the method of superposition to calculate the discharge vs. time relationship of debris flow is also studied. Test results show that saturation and seepage at the toe of the slope are signs of the beginning of intensive sand discharge. Two stages of the sand discharge curve are observed. The first stage show abrupt increase of the sand discharge associated the liquefaction of slope toe. The second stage show fluctuated sand discharge curves associated with retrogressive failure of the slope. Between the two factors examined, the rainfall intensity has a stronger influence on the time and peak value of sand discharge. The method of linear superposition seems to work well based on some limited flume and model slope test results. Ching-Chuan Huang 黃景川 2006 學位論文 ; thesis 85 zh-TW |
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碩士 === 國立暨南國際大學 === 地震與防災工程研究所 === 94 === Experiments on the development of debris flow using flume and slope model tests are performed to investigate the following two factors:(1) The density of soil and (2) Rainfall intensity. Feasibility of using the method of superposition to calculate the discharge vs. time relationship of debris flow is also studied.
Test results show that saturation and seepage at the toe of the slope are signs of the beginning of intensive sand discharge. Two stages of the sand discharge curve are observed. The first stage show abrupt increase of the sand discharge associated the liquefaction of slope toe. The second stage show fluctuated sand discharge curves associated with retrogressive failure of the slope. Between the two factors examined, the rainfall intensity has a stronger influence on the time and peak value of sand discharge. The method of linear superposition seems to work well based on some limited flume and model slope test results.
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author2 |
Ching-Chuan Huang |
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Ching-Chuan Huang Li-Kang Hu 胡立康 |
author |
Li-Kang Hu 胡立康 |
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Li-Kang Hu 胡立康 Model tests and analysis on development process of debris flow |
author_sort |
Li-Kang Hu |
title |
Model tests and analysis on development process of debris flow |
title_short |
Model tests and analysis on development process of debris flow |
title_full |
Model tests and analysis on development process of debris flow |
title_fullStr |
Model tests and analysis on development process of debris flow |
title_full_unstemmed |
Model tests and analysis on development process of debris flow |
title_sort |
model tests and analysis on development process of debris flow |
publishDate |
2006 |
url |
http://ndltd.ncl.edu.tw/handle/42103570850700513335 |
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