Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River

碩士 === 逢甲大學 === 土木及水利工程所 === 90 === In Taiwan most of the researches of tidal reach focused on Danshuei river system, at northern Taiwan especially for Keelung river. The experimental data (current velocity, discharge, water lever and salinity) influenced by tide are deficient for the other part o...

Full description

Bibliographic Details
Main Authors: Kung-Chung Jeng, 鄭坤忠
Other Authors: none
Format: Others
Language:zh-TW
Published: 2002
Online Access:http://ndltd.ncl.edu.tw/handle/qyr9ms
id ndltd-TW-090FCU05017028
record_format oai_dc
spelling ndltd-TW-090FCU050170282018-05-10T04:22:13Z http://ndltd.ncl.edu.tw/handle/qyr9ms Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River 烏溪感潮河段一維及二維延散係數之實測 Kung-Chung Jeng 鄭坤忠 碩士 逢甲大學 土木及水利工程所 90 In Taiwan most of the researches of tidal reach focused on Danshuei river system, at northern Taiwan especially for Keelung river. The experimental data (current velocity, discharge, water lever and salinity) influenced by tide are deficient for the other part of Taiwan. Wu-shi basin is important due to it''s geography, rich water resources, economy, population and wetland ecosystem. This thesis used salt transport analysis and longitudinal salt gradient collected by measuring cross-section, water lever, current velocity and salinity of Shi-Bin bridge to calculate instant 1-D dispersion coefficient K and tidal average 1-D dispersion coefficient <K>. 2-D transverse dispersion coefficient Ey is obtained by way of instantaneous tracer release. The field transverse concentration distribution is compared with that from diffusion equation of difference Ey to find an appropriate 2-D transverse dispersion coefficient. 2-D longitudinal dispersion coefficient Ex is calculated by theoretical formulate of Elder[22]. The result of this thesis, K is 2~-95 , <K> is —229 , dimensionless diffusion coefficient < > is 8262, and these values are much influenced by tidal intensity. From the salt transport analysis, the effects of tidal pumping, vertical shear dispersion and transverse shear dispersion are the major causes for the dispersion at the Shi-Bin bridge, while the effects of wind、topography and coriolis force are insignificant. Ex , Ey are 1.35 and 0.095 , dimensionless longitudinal and transverse diffusion , are 3 and 1.23 respectively. This thesis establishs 1-D and 2-D experimental procedures of tidal reach of Wu-Shi, analyzes transport mechanism and dispersion coefficient of 1-D and 2-D, and provides references for environmental developmental administration and for water quality model parameters. none 鄭仙偉 2002 學位論文 ; thesis 151 zh-TW
collection NDLTD
language zh-TW
format Others
sources NDLTD
description 碩士 === 逢甲大學 === 土木及水利工程所 === 90 === In Taiwan most of the researches of tidal reach focused on Danshuei river system, at northern Taiwan especially for Keelung river. The experimental data (current velocity, discharge, water lever and salinity) influenced by tide are deficient for the other part of Taiwan. Wu-shi basin is important due to it''s geography, rich water resources, economy, population and wetland ecosystem. This thesis used salt transport analysis and longitudinal salt gradient collected by measuring cross-section, water lever, current velocity and salinity of Shi-Bin bridge to calculate instant 1-D dispersion coefficient K and tidal average 1-D dispersion coefficient <K>. 2-D transverse dispersion coefficient Ey is obtained by way of instantaneous tracer release. The field transverse concentration distribution is compared with that from diffusion equation of difference Ey to find an appropriate 2-D transverse dispersion coefficient. 2-D longitudinal dispersion coefficient Ex is calculated by theoretical formulate of Elder[22]. The result of this thesis, K is 2~-95 , <K> is —229 , dimensionless diffusion coefficient < > is 8262, and these values are much influenced by tidal intensity. From the salt transport analysis, the effects of tidal pumping, vertical shear dispersion and transverse shear dispersion are the major causes for the dispersion at the Shi-Bin bridge, while the effects of wind、topography and coriolis force are insignificant. Ex , Ey are 1.35 and 0.095 , dimensionless longitudinal and transverse diffusion , are 3 and 1.23 respectively. This thesis establishs 1-D and 2-D experimental procedures of tidal reach of Wu-Shi, analyzes transport mechanism and dispersion coefficient of 1-D and 2-D, and provides references for environmental developmental administration and for water quality model parameters.
author2 none
author_facet none
Kung-Chung Jeng
鄭坤忠
author Kung-Chung Jeng
鄭坤忠
spellingShingle Kung-Chung Jeng
鄭坤忠
Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River
author_sort Kung-Chung Jeng
title Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River
title_short Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River
title_full Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River
title_fullStr Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River
title_full_unstemmed Measurement and Study of 1-D and 2-D Dispersion Coefficient in the Tidal Reach of Wu-Shi River
title_sort measurement and study of 1-d and 2-d dispersion coefficient in the tidal reach of wu-shi river
publishDate 2002
url http://ndltd.ncl.edu.tw/handle/qyr9ms
work_keys_str_mv AT kungchungjeng measurementandstudyof1dand2ddispersioncoefficientinthetidalreachofwushiriver
AT zhèngkūnzhōng measurementandstudyof1dand2ddispersioncoefficientinthetidalreachofwushiriver
AT kungchungjeng wūxīgǎncháohéduànyīwéijíèrwéiyánsànxìshùzhīshícè
AT zhèngkūnzhōng wūxīgǎncháohéduànyīwéijíèrwéiyánsànxìshùzhīshícè
_version_ 1718635446649487360