Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation

碩士 === 逢甲大學 === 土木及水利工程研究所 === 85 ===   MacCormack scheme is accessed in solving de St. Venant equations and one-dimensional advection-dispersion equation for the interior points of solution domain. For boundary points, method of characteristic line is employed. Mass conservation is checked and ca...

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Main Author: 溫至剛
Other Authors: 許少華
Format: Others
Language:zh-TW
Published: 1997
Online Access:http://ndltd.ncl.edu.tw/handle/38671998790953712156
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spelling ndltd-TW-085FCU030170012015-10-13T12:15:15Z http://ndltd.ncl.edu.tw/handle/38671998790953712156 Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation MacCormack法在定床渾水變量流模式之實用性探討 溫至剛 碩士 逢甲大學 土木及水利工程研究所 85   MacCormack scheme is accessed in solving de St. Venant equations and one-dimensional advection-dispersion equation for the interior points of solution domain. For boundary points, method of characteristic line is employed. Mass conservation is checked and cases of positive/negative surges with analytical solutions are employed to verify this numerical model. Artificial viscosity is found necessary in smoothing numerical oscillation inherited from this explicit, second order scheme. Cases of interesting phenomena are then tested to show the usefulness of this Scheme. No effort is needed to track the hydraulic discontinuity in the case of sudden change from supercritical to subcritical flow. Constrained by stability condition, the time step of MacCormack scheme is relatively small. 許少華 1997 學位論文 ; thesis 104 zh-TW
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language zh-TW
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description 碩士 === 逢甲大學 === 土木及水利工程研究所 === 85 ===   MacCormack scheme is accessed in solving de St. Venant equations and one-dimensional advection-dispersion equation for the interior points of solution domain. For boundary points, method of characteristic line is employed. Mass conservation is checked and cases of positive/negative surges with analytical solutions are employed to verify this numerical model. Artificial viscosity is found necessary in smoothing numerical oscillation inherited from this explicit, second order scheme. Cases of interesting phenomena are then tested to show the usefulness of this Scheme. No effort is needed to track the hydraulic discontinuity in the case of sudden change from supercritical to subcritical flow. Constrained by stability condition, the time step of MacCormack scheme is relatively small.
author2 許少華
author_facet 許少華
溫至剛
author 溫至剛
spellingShingle 溫至剛
Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation
author_sort 溫至剛
title Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation
title_short Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation
title_full Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation
title_fullStr Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation
title_full_unstemmed Accessment of MacCormack Scheme in Unsteady Sediment-laden Flow Computation
title_sort accessment of maccormack scheme in unsteady sediment-laden flow computation
publishDate 1997
url http://ndltd.ncl.edu.tw/handle/38671998790953712156
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