Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou
碩士 === 國立臺灣大學 === 森林環境暨資源學研究所 === 96 === The aim of this study is to investigate the colluvium characteristics using electric resistivity method at University gulley in Chitou. The resistivities and the layer depths can figure the geological and hydraulic condition in this area. The offset errors by...
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ndltd-TW-096NTU053590082016-05-11T04:16:52Z http://ndltd.ncl.edu.tw/handle/48856957400265223657 Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou 大地比電阻法應用於溪頭大學坑崩塌地之調查 Jheng-Tang Ciou 邱正唐 碩士 國立臺灣大學 森林環境暨資源學研究所 96 The aim of this study is to investigate the colluvium characteristics using electric resistivity method at University gulley in Chitou. The resistivities and the layer depths can figure the geological and hydraulic condition in this area. The offset errors by the arranged arrays can estimate the lateral resistivity effects in the landslide site. The findings are as follows: 1. Analyzing the resistivity tomography, the accumulated composition in the colluvium is discontinuous and loose. 2. The low resistivity layers, says the subsurface flow or clay layers, found in dry and wet periods may endanger this site in the rain seasons. 3. Investigating from the upper to the lower slopes, the resistivity tomographies and the offset errors show the geological characteristics of debris flow. 4. The offset errors indicate the influence of the heterogenic to the survey is large. 陳信雄 2008 學位論文 ; thesis 58 zh-TW |
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碩士 === 國立臺灣大學 === 森林環境暨資源學研究所 === 96 === The aim of this study is to investigate the colluvium characteristics using electric resistivity method at University gulley in Chitou. The resistivities and the layer depths can figure the geological and hydraulic condition in this area. The offset errors by the arranged arrays can estimate the lateral resistivity effects in the landslide site. The findings are as follows:
1. Analyzing the resistivity tomography, the accumulated composition in the colluvium is discontinuous and loose.
2. The low resistivity layers, says the subsurface flow or clay layers, found in dry and wet periods may endanger this site in the rain seasons.
3. Investigating from the upper to the lower slopes, the resistivity tomographies and the offset errors show the geological characteristics of debris flow.
4. The offset errors indicate the influence of the heterogenic to the survey is large.
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author2 |
陳信雄 |
author_facet |
陳信雄 Jheng-Tang Ciou 邱正唐 |
author |
Jheng-Tang Ciou 邱正唐 |
spellingShingle |
Jheng-Tang Ciou 邱正唐 Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou |
author_sort |
Jheng-Tang Ciou |
title |
Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou |
title_short |
Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou |
title_full |
Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou |
title_fullStr |
Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou |
title_full_unstemmed |
Application of Electric Resistivity Method to Landslide Survey at University Gulley in Chitou |
title_sort |
application of electric resistivity method to landslide survey at university gulley in chitou |
publishDate |
2008 |
url |
http://ndltd.ncl.edu.tw/handle/48856957400265223657 |
work_keys_str_mv |
AT jhengtangciou applicationofelectricresistivitymethodtolandslidesurveyatuniversitygulleyinchitou AT qiūzhèngtáng applicationofelectricresistivitymethodtolandslidesurveyatuniversitygulleyinchitou AT jhengtangciou dàdebǐdiànzǔfǎyīngyòngyúxītóudàxuékēngbēngtādezhīdiàochá AT qiūzhèngtáng dàdebǐdiànzǔfǎyīngyòngyúxītóudàxuékēngbēngtādezhīdiàochá |
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1718265503153127424 |