A Study on the Stability of Chung-Xin-Tzu No.2 Landslide

碩士 === 國立中興大學 === 水土保持學系 === 87 === Nan Tou situats at central of Taiwan . Because it has many mountains , high density of erosion and geology is brittle , So hillside fields often occur erosion by harmful drainage caused area of 7 ha . By theoretical analyses , investigation , laboratory and fiel...

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Main Authors: Kuo Chang Tseng, 曾國彰
Other Authors: Han-Jung Shieh
Format: Others
Language:zh-TW
Published: 1999
Online Access:http://ndltd.ncl.edu.tw/handle/15915972744829394404
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spelling ndltd-TW-087NCHU00800202016-02-03T04:32:45Z http://ndltd.ncl.edu.tw/handle/15915972744829394404 A Study on the Stability of Chung-Xin-Tzu No.2 Landslide 中心仔二號地滑地穩定性之探討 Kuo Chang Tseng 曾國彰 碩士 國立中興大學 水土保持學系 87 Nan Tou situats at central of Taiwan . Because it has many mountains , high density of erosion and geology is brittle , So hillside fields often occur erosion by harmful drainage caused area of 7 ha . By theoretical analyses , investigation , laboratory and field tests , the result were summarized as follow : (一) Many factors involved in landslide , it includes weak topography , soil erosion and bad surface drainage , That give rise lower region to collapse and cause landslide . (二) Composited of geological structure and strain’s value and a analysis of landslide depth . It can shows hillside slope stability analysis . If it can strengthen surface drainage and dredge erosion tunnel , calamity does not occur easily . (三) Many regions have slope stability except toe of landslide is still change . So it must plan prevent treatment and still proceed periodical observation . (四) Analysis of hydrological information , we have forecast equation as follow : qi=(2*R*0.24)/(1.0013+3.0011) R: volume of rainfall per day qi:volume of groundwater Han-Jung Shieh 謝豪榮 1999 學位論文 ; thesis 150 zh-TW
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language zh-TW
format Others
sources NDLTD
description 碩士 === 國立中興大學 === 水土保持學系 === 87 === Nan Tou situats at central of Taiwan . Because it has many mountains , high density of erosion and geology is brittle , So hillside fields often occur erosion by harmful drainage caused area of 7 ha . By theoretical analyses , investigation , laboratory and field tests , the result were summarized as follow : (一) Many factors involved in landslide , it includes weak topography , soil erosion and bad surface drainage , That give rise lower region to collapse and cause landslide . (二) Composited of geological structure and strain’s value and a analysis of landslide depth . It can shows hillside slope stability analysis . If it can strengthen surface drainage and dredge erosion tunnel , calamity does not occur easily . (三) Many regions have slope stability except toe of landslide is still change . So it must plan prevent treatment and still proceed periodical observation . (四) Analysis of hydrological information , we have forecast equation as follow : qi=(2*R*0.24)/(1.0013+3.0011) R: volume of rainfall per day qi:volume of groundwater
author2 Han-Jung Shieh
author_facet Han-Jung Shieh
Kuo Chang Tseng
曾國彰
author Kuo Chang Tseng
曾國彰
spellingShingle Kuo Chang Tseng
曾國彰
A Study on the Stability of Chung-Xin-Tzu No.2 Landslide
author_sort Kuo Chang Tseng
title A Study on the Stability of Chung-Xin-Tzu No.2 Landslide
title_short A Study on the Stability of Chung-Xin-Tzu No.2 Landslide
title_full A Study on the Stability of Chung-Xin-Tzu No.2 Landslide
title_fullStr A Study on the Stability of Chung-Xin-Tzu No.2 Landslide
title_full_unstemmed A Study on the Stability of Chung-Xin-Tzu No.2 Landslide
title_sort study on the stability of chung-xin-tzu no.2 landslide
publishDate 1999
url http://ndltd.ncl.edu.tw/handle/15915972744829394404
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