Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees
博士 === 國立成功大學 === 水利及海洋工程學系 === 88 === The present paper is aimed to develop a numerical model based on an explicit finite-difference method for simulating unsteady flow and bed variations in alluvial rivers. A set of experimental data on channel-contraction is used to examine the ability of this mo...
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ndltd-TW-088NCKU00830552015-10-13T12:47:24Z http://ndltd.ncl.edu.tw/handle/20260358264046841450 Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees 定岸沖積河流水理及底床演變之模擬 Chih-Heng Tsai 蔡智恆 博士 國立成功大學 水利及海洋工程學系 88 The present paper is aimed to develop a numerical model based on an explicit finite-difference method for simulating unsteady flow and bed variations in alluvial rivers. A set of experimental data on channel-contraction is used to examine the ability of this model. The numerical results are satisfactory, as clearly observed from comparisons with measured data. Also, two bed-load formulas are chosen for simulating the experiment. The findings indicate that quantitative effect is the influence of the bed-load formula on bed evolution. The applicability of the model can be performed by simulating the bed evolution of Tseng-Wen River during flood stage. The main-channel would occur intense erosion and form a larger cross-section in the earlier stage of swell. At the same time, the flood-plains far away from the main-channel would silt. Furthermore, the suspended-sediment concentration of the main-channel is more heavy and more uniform in the transverse direction, as compared to that of flood-plains. Chang-Tai Tsai 蔡長泰 2000 學位論文 ; thesis 209 zh-TW |
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博士 === 國立成功大學 === 水利及海洋工程學系 === 88 === The present paper is aimed to develop a numerical model based on an explicit finite-difference method for simulating unsteady flow and bed variations in alluvial rivers. A set of experimental data on channel-contraction is used to examine the ability of this model. The numerical results are satisfactory, as clearly observed from comparisons with measured data. Also, two bed-load formulas are chosen for simulating the experiment. The findings indicate that quantitative effect is the influence of the bed-load formula on bed evolution. The applicability of the model can be performed by simulating the bed evolution of Tseng-Wen River during flood stage. The main-channel would occur intense erosion and form a larger cross-section in the earlier stage of swell. At the same time, the flood-plains far away from the main-channel would silt. Furthermore, the suspended-sediment concentration of the main-channel is more heavy and more uniform in the transverse direction, as compared to that of flood-plains.
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author2 |
Chang-Tai Tsai |
author_facet |
Chang-Tai Tsai Chih-Heng Tsai 蔡智恆 |
author |
Chih-Heng Tsai 蔡智恆 |
spellingShingle |
Chih-Heng Tsai 蔡智恆 Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees |
author_sort |
Chih-Heng Tsai |
title |
Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees |
title_short |
Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees |
title_full |
Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees |
title_fullStr |
Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees |
title_full_unstemmed |
Numerical Simulation of Flow and Bed Evolution in Alluvial River with Levees |
title_sort |
numerical simulation of flow and bed evolution in alluvial river with levees |
publishDate |
2000 |
url |
http://ndltd.ncl.edu.tw/handle/20260358264046841450 |
work_keys_str_mv |
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