Observations on jet flipping below a sluice gate

It is a necessary to investigate effects of scour downstream of many hydraulic structures, especially in an erodible sediment bed below that structures. This explains the reason why we need to get deeper understanding about the intense local bed degradation by observing the scour characteristics in...

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Main Author: Thuy, Nguyen Thanh
Other Authors: Lim Siow Yong
Format: Final Year Project
Language:English
Published: 2014
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Online Access:http://hdl.handle.net/10356/61177
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-611772019-12-10T12:47:00Z Observations on jet flipping below a sluice gate Thuy, Nguyen Thanh Lim Siow Yong School of Civil and Environmental Engineering DRNTU::Engineering It is a necessary to investigate effects of scour downstream of many hydraulic structures, especially in an erodible sediment bed below that structures. This explains the reason why we need to get deeper understanding about the intense local bed degradation by observing the scour characteristics in this project. Experiments were carried out on scour downstream of a sluice gate with varying apron length. The runs were recorded and the scour characteristics as well as a jet flipping phenomenon were studied via the recorded videos. Most of the runs have an appearance of jet flipping except the runs where the apron lengths are extremely short or extremely long. The flow pattern depends on the apron length and it is showed that there is a critical range of apron lengths along which jet flipping would occur and beyond this range we cannot observe any jet flipping phenomenon. The interchange between water jet direction, from bed to water surface and vice versa, makes the jet flipping phenomenon happen. The scour hole is formed before the jet flipping is observed and the shape of scour hole is continuously changed during scouring process with different apron length per each cycle. Each cycle consists of a digging phase and a filling phase. The digging phase creates a scour hole while the filling phase fills the hole until the next jet flipping cycle with the dig-fill processes being repeated. In this study, the starting time and ending time of digging phase and filling phase of every cycle were taken down. The scour hole shapes in the end of each phase were captured and its volume were calculated. And there are discussions about the collective effects of parameters such as tail water depth, water jet velocity and apron length in the occurrence and frequency of jet flipping. There are also numerous diagrams, which were created from extracted data using WinDIG, and are useful to describe the flow directions, velocity distribution and centreline scour profiles during the digging phase and the filling phase. These diagrams provide clearer visualisation of the flow fields, therefore, the jet-flipping phenomenon could be understood better. Bachelor of Engineering (Environmental Engineering) 2014-06-06T01:24:00Z 2014-06-06T01:24:00Z 2014 2014 Final Year Project (FYP) http://hdl.handle.net/10356/61177 en Nanyang Technological University 47 p. application/msword
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic DRNTU::Engineering
spellingShingle DRNTU::Engineering
Thuy, Nguyen Thanh
Observations on jet flipping below a sluice gate
description It is a necessary to investigate effects of scour downstream of many hydraulic structures, especially in an erodible sediment bed below that structures. This explains the reason why we need to get deeper understanding about the intense local bed degradation by observing the scour characteristics in this project. Experiments were carried out on scour downstream of a sluice gate with varying apron length. The runs were recorded and the scour characteristics as well as a jet flipping phenomenon were studied via the recorded videos. Most of the runs have an appearance of jet flipping except the runs where the apron lengths are extremely short or extremely long. The flow pattern depends on the apron length and it is showed that there is a critical range of apron lengths along which jet flipping would occur and beyond this range we cannot observe any jet flipping phenomenon. The interchange between water jet direction, from bed to water surface and vice versa, makes the jet flipping phenomenon happen. The scour hole is formed before the jet flipping is observed and the shape of scour hole is continuously changed during scouring process with different apron length per each cycle. Each cycle consists of a digging phase and a filling phase. The digging phase creates a scour hole while the filling phase fills the hole until the next jet flipping cycle with the dig-fill processes being repeated. In this study, the starting time and ending time of digging phase and filling phase of every cycle were taken down. The scour hole shapes in the end of each phase were captured and its volume were calculated. And there are discussions about the collective effects of parameters such as tail water depth, water jet velocity and apron length in the occurrence and frequency of jet flipping. There are also numerous diagrams, which were created from extracted data using WinDIG, and are useful to describe the flow directions, velocity distribution and centreline scour profiles during the digging phase and the filling phase. These diagrams provide clearer visualisation of the flow fields, therefore, the jet-flipping phenomenon could be understood better.
author2 Lim Siow Yong
author_facet Lim Siow Yong
Thuy, Nguyen Thanh
format Final Year Project
author Thuy, Nguyen Thanh
author_sort Thuy, Nguyen Thanh
title Observations on jet flipping below a sluice gate
title_short Observations on jet flipping below a sluice gate
title_full Observations on jet flipping below a sluice gate
title_fullStr Observations on jet flipping below a sluice gate
title_full_unstemmed Observations on jet flipping below a sluice gate
title_sort observations on jet flipping below a sluice gate
publishDate 2014
url http://hdl.handle.net/10356/61177
_version_ 1681041080867356672