Effect of Lateral Inflow on Meandering Channel Flow
碩士 === 國立交通大學 === 土木工程系所 === 103 === Natural rivers with meanders and confluences have complicated patterns of flows and sediment transport behaviors, in which disasters may be frequently induced. In junction regions between main stream and branches, momentum transitions often cause dramatic changes...
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ndltd-TW-103NCTU50150752016-08-12T04:14:06Z http://ndltd.ncl.edu.tw/handle/21951032995009187495 Effect of Lateral Inflow on Meandering Channel Flow 蜿蜒渠流受側入流影響之探討 Tsung-Yuan Yang 楊宗原 碩士 國立交通大學 土木工程系所 103 Natural rivers with meanders and confluences have complicated patterns of flows and sediment transport behaviors, in which disasters may be frequently induced. In junction regions between main stream and branches, momentum transitions often cause dramatic changes in flow conditions and getting more severe with higher levels of meandering. And therefore, by following that the instability of bed evolution induced by the dramatic change of sediment movement may inflict the severe damage on the flood-proof infrastuctures. The main purpose of this study is to investigate the changes of flow characteristics in a meaderning channel with the introduction of lateral flows. Experiments were conducted to investigate the flow behaviors in junctions and along channels. Velocity measurements were taken using an acoustic doppler velocimeter over a gridded junction region. The simulation results of a 3D model (RESED3D) showed well agreement with the experimental data. Furthermore, this study investigates the differences in velocity distribution and water depth distribution between the meandering channels with and without lateral flows. Jinn-Chuang Yang 楊錦釧 2015 學位論文 ; thesis 80 zh-TW |
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碩士 === 國立交通大學 === 土木工程系所 === 103 === Natural rivers with meanders and confluences have complicated patterns of flows and sediment transport behaviors, in which disasters may be frequently induced. In junction regions between main stream and branches, momentum transitions often cause dramatic changes in flow conditions and getting more severe with higher levels of meandering. And therefore, by following that the instability of bed evolution induced by the dramatic change of sediment movement may inflict the severe damage on the flood-proof infrastuctures.
The main purpose of this study is to investigate the changes of flow characteristics in a meaderning channel with the introduction of lateral flows. Experiments were conducted to investigate the flow behaviors in junctions and along channels. Velocity measurements were taken using an acoustic doppler velocimeter over a gridded junction region. The simulation results of a 3D model (RESED3D) showed well agreement with the experimental data. Furthermore, this study investigates the differences in velocity distribution and water depth distribution between the meandering channels with and without lateral flows.
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author2 |
Jinn-Chuang Yang |
author_facet |
Jinn-Chuang Yang Tsung-Yuan Yang 楊宗原 |
author |
Tsung-Yuan Yang 楊宗原 |
spellingShingle |
Tsung-Yuan Yang 楊宗原 Effect of Lateral Inflow on Meandering Channel Flow |
author_sort |
Tsung-Yuan Yang |
title |
Effect of Lateral Inflow on Meandering Channel Flow |
title_short |
Effect of Lateral Inflow on Meandering Channel Flow |
title_full |
Effect of Lateral Inflow on Meandering Channel Flow |
title_fullStr |
Effect of Lateral Inflow on Meandering Channel Flow |
title_full_unstemmed |
Effect of Lateral Inflow on Meandering Channel Flow |
title_sort |
effect of lateral inflow on meandering channel flow |
publishDate |
2015 |
url |
http://ndltd.ncl.edu.tw/handle/21951032995009187495 |
work_keys_str_mv |
AT tsungyuanyang effectoflateralinflowonmeanderingchannelflow AT yángzōngyuán effectoflateralinflowonmeanderingchannelflow AT tsungyuanyang wānyánqúliúshòucèrùliúyǐngxiǎngzhītàntǎo AT yángzōngyuán wānyánqúliúshòucèrùliúyǐngxiǎngzhītàntǎo |
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