Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave

碩士 === 國立中興大學 === 土木工程學系所 === 96 === The purpose of this study is to understand the flow field of internal solitary wave running up and down along a sloping bottom. The experiments of internal solitary waves were carried out using stratified two-layer fresh/saline water in the wave flume. The slope...

Full description

Bibliographic Details
Main Authors: Jen-Shiun Lin, 林振勛
Other Authors: 林呈
Format: Others
Language:zh-TW
Published: 2008
Online Access:http://ndltd.ncl.edu.tw/handle/99404161979994356865
id ndltd-TW-096NCHU5015108
record_format oai_dc
spelling ndltd-TW-096NCHU50151082016-05-09T04:13:52Z http://ndltd.ncl.edu.tw/handle/99404161979994356865 Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave 於斜坡上傳輸之上舉型孤立內波特性之實驗研究 Jen-Shiun Lin 林振勛 碩士 國立中興大學 土木工程學系所 96 The purpose of this study is to understand the flow field of internal solitary wave running up and down along a sloping bottom. The experiments of internal solitary waves were carried out using stratified two-layer fresh/saline water in the wave flume. The slope of sloping-bottom model was set with a fixed angle of 30 °. The experiments were conducted under the same density ratio ( ) and the same thickness ratio of the upper and lower layers (h1/h2 = 7). The internal solitary waves were generated by changing different potential energies ( = 5 cm, 10 cm, 15 cm, and 20 cm). The dye was added into water for flow visualization. The particle image velocimetry (PIV) was used to measure quantitatively the velocity distribution of internal solitary waves. The high-speed camera was used to capture the images of flow field. The validations of the incident internal solitary wave was carried out in absence of obstacle. Good agreement was obtained from the comparison between the wave shape of the internal solitary wave and the Kdv or mKdv theory. The horizontal velocity was validated by using FLDV. The wave propagation processes, including run-up and run-down, were observed by flow visualization. The measuring coordinate was tilted to an angle of 30 ° for the measurement of velocity distribution along the slope. The characteristics of velocity profile were investigated in detail with dimensionless time T during the run-up and run-down processes. Using shear layer concept proposed by Lin et al. (2008), velocity distribution of the internal solitary wave was analyzed for run-up and run-down processes. The velocity and length scales were clearly defined using hyperbolic tangent function. The similarity profile of velocity distribution for shear layer has been found in the study. 林呈 2008 學位論文 ; thesis 79 zh-TW
collection NDLTD
language zh-TW
format Others
sources NDLTD
description 碩士 === 國立中興大學 === 土木工程學系所 === 96 === The purpose of this study is to understand the flow field of internal solitary wave running up and down along a sloping bottom. The experiments of internal solitary waves were carried out using stratified two-layer fresh/saline water in the wave flume. The slope of sloping-bottom model was set with a fixed angle of 30 °. The experiments were conducted under the same density ratio ( ) and the same thickness ratio of the upper and lower layers (h1/h2 = 7). The internal solitary waves were generated by changing different potential energies ( = 5 cm, 10 cm, 15 cm, and 20 cm). The dye was added into water for flow visualization. The particle image velocimetry (PIV) was used to measure quantitatively the velocity distribution of internal solitary waves. The high-speed camera was used to capture the images of flow field. The validations of the incident internal solitary wave was carried out in absence of obstacle. Good agreement was obtained from the comparison between the wave shape of the internal solitary wave and the Kdv or mKdv theory. The horizontal velocity was validated by using FLDV. The wave propagation processes, including run-up and run-down, were observed by flow visualization. The measuring coordinate was tilted to an angle of 30 ° for the measurement of velocity distribution along the slope. The characteristics of velocity profile were investigated in detail with dimensionless time T during the run-up and run-down processes. Using shear layer concept proposed by Lin et al. (2008), velocity distribution of the internal solitary wave was analyzed for run-up and run-down processes. The velocity and length scales were clearly defined using hyperbolic tangent function. The similarity profile of velocity distribution for shear layer has been found in the study.
author2 林呈
author_facet 林呈
Jen-Shiun Lin
林振勛
author Jen-Shiun Lin
林振勛
spellingShingle Jen-Shiun Lin
林振勛
Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave
author_sort Jen-Shiun Lin
title Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave
title_short Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave
title_full Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave
title_fullStr Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave
title_full_unstemmed Experimental Study on the Characteristics of Flow Induced by an Internal Solitary Shoaling Wave
title_sort experimental study on the characteristics of flow induced by an internal solitary shoaling wave
publishDate 2008
url http://ndltd.ncl.edu.tw/handle/99404161979994356865
work_keys_str_mv AT jenshiunlin experimentalstudyonthecharacteristicsofflowinducedbyaninternalsolitaryshoalingwave
AT línzhènxūn experimentalstudyonthecharacteristicsofflowinducedbyaninternalsolitaryshoalingwave
AT jenshiunlin yúxiépōshàngchuánshūzhīshàngjǔxínggūlìnèibōtèxìngzhīshíyànyánjiū
AT línzhènxūn yúxiépōshàngchuánshūzhīshàngjǔxínggūlìnèibōtèxìngzhīshíyànyánjiū
_version_ 1718262555726577664