Evolution of a deep-seated creeping slope and associated characteristics: A case stud

碩士 === 國立臺北科技大學 === 資源工程研究所 === 101 === The deep-seated slope movement is the one characterized by a huge scope moving mass with a deep sliding surface, low displacement rate, or a connecting of several moving masses with deep sliding surfaces. The existence how to affirm the deep-seated slope is an...

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Main Authors: Bai-Chiao Lo, 羅百喬
Other Authors: 翁祖炘
Format: Others
Language:zh-TW
Published: 2013
Online Access:http://ndltd.ncl.edu.tw/handle/55d4ez
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spelling ndltd-TW-101TIT053970262019-05-15T21:02:31Z http://ndltd.ncl.edu.tw/handle/55d4ez Evolution of a deep-seated creeping slope and associated characteristics: A case stud 深層地滑邊坡運動歷程暨微地動特性案例研究 Bai-Chiao Lo 羅百喬 碩士 國立臺北科技大學 資源工程研究所 101 The deep-seated slope movement is the one characterized by a huge scope moving mass with a deep sliding surface, low displacement rate, or a connecting of several moving masses with deep sliding surfaces. The existence how to affirm the deep-seated slope is an important project of domestic side slope disaster prevention and control with sliding range. A deep-seated slope movement case with many years monitoring data and 50 years of aerial photograph in southeast Taiwan, this article investigates the site characteristics of the slope. Borehole investigations, collecting monitoring and identification aerial photograph revealed the presence of unstably slope, which when integrated with inclinometer, image-mosaic technology detecting lining cracks and surface geodetic data, helped to provide key insights into the underlying instability mechanisms. Surface and borehole investigations of the unstable mass reveal an up to 90 m deep of metamorphic rocks divided into three primary blocks. The result showed deep-seated slope tended to move towards toe of slope and discontinuity attitude .The different response of microseismic measurement can make a distinction of slip the region and outside. 翁祖炘 王泰典 2013 學位論文 ; thesis 160 zh-TW
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language zh-TW
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description 碩士 === 國立臺北科技大學 === 資源工程研究所 === 101 === The deep-seated slope movement is the one characterized by a huge scope moving mass with a deep sliding surface, low displacement rate, or a connecting of several moving masses with deep sliding surfaces. The existence how to affirm the deep-seated slope is an important project of domestic side slope disaster prevention and control with sliding range. A deep-seated slope movement case with many years monitoring data and 50 years of aerial photograph in southeast Taiwan, this article investigates the site characteristics of the slope. Borehole investigations, collecting monitoring and identification aerial photograph revealed the presence of unstably slope, which when integrated with inclinometer, image-mosaic technology detecting lining cracks and surface geodetic data, helped to provide key insights into the underlying instability mechanisms. Surface and borehole investigations of the unstable mass reveal an up to 90 m deep of metamorphic rocks divided into three primary blocks. The result showed deep-seated slope tended to move towards toe of slope and discontinuity attitude .The different response of microseismic measurement can make a distinction of slip the region and outside.
author2 翁祖炘
author_facet 翁祖炘
Bai-Chiao Lo
羅百喬
author Bai-Chiao Lo
羅百喬
spellingShingle Bai-Chiao Lo
羅百喬
Evolution of a deep-seated creeping slope and associated characteristics: A case stud
author_sort Bai-Chiao Lo
title Evolution of a deep-seated creeping slope and associated characteristics: A case stud
title_short Evolution of a deep-seated creeping slope and associated characteristics: A case stud
title_full Evolution of a deep-seated creeping slope and associated characteristics: A case stud
title_fullStr Evolution of a deep-seated creeping slope and associated characteristics: A case stud
title_full_unstemmed Evolution of a deep-seated creeping slope and associated characteristics: A case stud
title_sort evolution of a deep-seated creeping slope and associated characteristics: a case stud
publishDate 2013
url http://ndltd.ncl.edu.tw/handle/55d4ez
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