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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Main Authors: Chih-Heng Tsai, 蔡智恆
Other Authors: Chang-Tai Tsai
Format: Others
Language:zh-TW
Published: 2000
Online Access:http://ndltd.ncl.edu.tw/handle/20260358264046841450
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spelling 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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description 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.
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
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