A Numerical Simulation of Onshore-Offshore Sediment Transport

碩士 === 淡江大學 === 水資源及環境工程所 === 82 === The incident waves on the beach and subsequent uprush and backwash change the beach profile,due to the sedimentation. This study is to develope a numerical model to calculate the onshore-offshore sedimen...

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Main Authors: Shi-Ming Tang, 唐世民
Other Authors: I-Chen Lin
Format: Others
Language:zh-TW
Published: 1993
Online Access:http://ndltd.ncl.edu.tw/handle/72510177676120898122
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spelling ndltd-TW-082TKU000870492016-02-08T04:06:32Z http://ndltd.ncl.edu.tw/handle/72510177676120898122 A Numerical Simulation of Onshore-Offshore Sediment Transport 在斜坡面上向離岸輸沙運移之數值模擬 Shi-Ming Tang 唐世民 碩士 淡江大學 水資源及環境工程所 82 The incident waves on the beach and subsequent uprush and backwash change the beach profile,due to the sedimentation. This study is to develope a numerical model to calculate the onshore-offshore sediment on a sandy beach,which includes hydrody- namic model and sedimentation model. Meyer & Taylor (1972) pointed out that the shallow water wave theory can adequately simulate the wave uprush phenomenon.Using Hibberd & Pereg- rine (1979)'s numerical model which is based on the shallow water wave theory this study developed a numerical scheme to simulate the phenomenon of wave uprush & backwash process can only be modelled by the idea of Ho & Mayer(1962), who have found that the major backwash mechanism was based on the free falling motion.The wave runup on a sloping beach is thus being simulated. As for the sedimentation model,the concept of total load developed by Bagnold(1966) is used.this numerical model has also taken into consideration of the changes of the beach profile.The wave is periodic and the sand grain is uniform.An equilib- rium beach can be found by the simulating result. The relation between erosion rate and bar steepness has been studied. The effects of some important parameters on the sedimentation on this sandy beach are also considered. I-Chen Lin 林意楨 1993 學位論文 ; thesis 3 zh-TW
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language zh-TW
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description 碩士 === 淡江大學 === 水資源及環境工程所 === 82 === The incident waves on the beach and subsequent uprush and backwash change the beach profile,due to the sedimentation. This study is to develope a numerical model to calculate the onshore-offshore sediment on a sandy beach,which includes hydrody- namic model and sedimentation model. Meyer & Taylor (1972) pointed out that the shallow water wave theory can adequately simulate the wave uprush phenomenon.Using Hibberd & Pereg- rine (1979)'s numerical model which is based on the shallow water wave theory this study developed a numerical scheme to simulate the phenomenon of wave uprush & backwash process can only be modelled by the idea of Ho & Mayer(1962), who have found that the major backwash mechanism was based on the free falling motion.The wave runup on a sloping beach is thus being simulated. As for the sedimentation model,the concept of total load developed by Bagnold(1966) is used.this numerical model has also taken into consideration of the changes of the beach profile.The wave is periodic and the sand grain is uniform.An equilib- rium beach can be found by the simulating result. The relation between erosion rate and bar steepness has been studied. The effects of some important parameters on the sedimentation on this sandy beach are also considered.
author2 I-Chen Lin
author_facet I-Chen Lin
Shi-Ming Tang
唐世民
author Shi-Ming Tang
唐世民
spellingShingle Shi-Ming Tang
唐世民
A Numerical Simulation of Onshore-Offshore Sediment Transport
author_sort Shi-Ming Tang
title A Numerical Simulation of Onshore-Offshore Sediment Transport
title_short A Numerical Simulation of Onshore-Offshore Sediment Transport
title_full A Numerical Simulation of Onshore-Offshore Sediment Transport
title_fullStr A Numerical Simulation of Onshore-Offshore Sediment Transport
title_full_unstemmed A Numerical Simulation of Onshore-Offshore Sediment Transport
title_sort numerical simulation of onshore-offshore sediment transport
publishDate 1993
url http://ndltd.ncl.edu.tw/handle/72510177676120898122
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