The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River

碩士 === 國立臺灣大學 === 地質科學研究所 === 96 === Jhoukou River is one of the branches of the Laonong River, and the most featured fluvial form is ingrown meander. Because of the strongly erosion along the Jhoukou River, there are some traces of channel migration. In this study, the channel centerline drawn from...

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Bibliographic Details
Main Authors:	Chia-Ming Hsu, 許家銘
Other Authors:	陳宏宇
Format:	Others
Language:	zh-TW
Published:	2008
Online Access:	http://ndltd.ncl.edu.tw/handle/60639527219147864253

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spelling	ndltd-TW-096NTU051380232016-05-11T04:17:10Z http://ndltd.ncl.edu.tw/handle/60639527219147864253 The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River 濁口溪流域的地表作用與地質環境間之相對應關係 Chia-Ming Hsu 許家銘碩士國立臺灣大學地質科學研究所 96 Jhoukou River is one of the branches of the Laonong River, and the most featured fluvial form is ingrown meander. Because of the strongly erosion along the Jhoukou River, there are some traces of channel migration. In this study, the channel centerline drawn from the air photos and SPOT satellite images is used to discover how the river changed and find out how landslides affect the meander. As for landslides, we use different SPOT satellite images to compute landslide ratio including typhoon Herb(1996), typhoon Bilis(2000), typhoon Toraji(2001), typhoon Mindulle(2004), and typhoon Haitang(2005). Sediment discharge during typhoon Mindulle is the lowest , and during typhoon Herb is the highest , respectively 0.36 Mt/y and 3.94 Mt/y. The average sediment discharge is 1.33 Mt/y from 1989 to 2005. 陳宏宇 2008 學位論文 ; thesis 80 zh-TW
collection	NDLTD
language	zh-TW
format	Others
sources	NDLTD
description	碩士 === 國立臺灣大學 === 地質科學研究所 === 96 === Jhoukou River is one of the branches of the Laonong River, and the most featured fluvial form is ingrown meander. Because of the strongly erosion along the Jhoukou River, there are some traces of channel migration. In this study, the channel centerline drawn from the air photos and SPOT satellite images is used to discover how the river changed and find out how landslides affect the meander. As for landslides, we use different SPOT satellite images to compute landslide ratio including typhoon Herb(1996), typhoon Bilis(2000), typhoon Toraji(2001), typhoon Mindulle(2004), and typhoon Haitang(2005). Sediment discharge during typhoon Mindulle is the lowest , and during typhoon Herb is the highest , respectively 0.36 Mt/y and 3.94 Mt/y. The average sediment discharge is 1.33 Mt/y from 1989 to 2005.
author2	陳宏宇
author_facet	陳宏宇 Chia-Ming Hsu 許家銘
author	Chia-Ming Hsu 許家銘
spellingShingle	Chia-Ming Hsu 許家銘 The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River
author_sort	Chia-Ming Hsu
title	The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River
title_short	The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River
title_full	The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River
title_fullStr	The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River
title_full_unstemmed	The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River
title_sort	relationship between earth processes and geological environmnet along the catchment of the jhuokou river
publishDate	2008
url	http://ndltd.ncl.edu.tw/handle/60639527219147864253
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The relationship between earth processes and geological environmnet along the catchment of the Jhuokou River

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