Characteristics of seismic signal and self-potentialof slope failure
碩士 === 國立中興大學 === 水土保持學系所 === 103 === It often occurs extreme rainfall that causes more landslide disasters in Taiwan. Before landslide happen, there will be changed in internal stratigraphic that cause self-potential changing and generate seismic signal. Therefore, this study in order to verify the...
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ndltd-TW-103NCHU50800362016-08-15T04:17:59Z http://ndltd.ncl.edu.tw/handle/61980213290715648347 Characteristics of seismic signal and self-potentialof slope failure 利用震動訊號及自然電位特性探討崩塌破壞 Bo-siang Lin 林博翔 碩士 國立中興大學 水土保持學系所 103 It often occurs extreme rainfall that causes more landslide disasters in Taiwan. Before landslide happen, there will be changed in internal stratigraphic that cause self-potential changing and generate seismic signal. Therefore, this study in order to verify the situation, and indoor slope model test conducted landslide test, and use control factor of rising groundwater and rainfall to observe self-potential changing and seismic signal during the test. The research results showed self-potential can reaction groundwater flow. In a continuous landslide process, it may correspond with the self-potential and seismic signal on the process. The research goal is determined whether the signals can be applied landslide warning before it destroyed, or it creates a new way to measure. It provides a new way for landslide monitoring and early warning. Zheng-Yi Feng 馮正一 2015 學位論文 ; thesis 79 zh-TW |
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碩士 === 國立中興大學 === 水土保持學系所 === 103 === It often occurs extreme rainfall that causes more landslide disasters in Taiwan. Before landslide happen, there will be changed in internal stratigraphic that cause self-potential changing and generate seismic signal. Therefore, this study in order to verify the situation, and indoor slope model test conducted landslide test, and use control factor of rising groundwater and rainfall to observe self-potential changing and seismic signal during the test. The research results showed self-potential can reaction groundwater flow. In a continuous landslide process, it may correspond with the self-potential and seismic signal on the process. The research goal is determined whether the signals can be applied landslide warning before it destroyed, or it creates a new way to measure. It provides a new way for landslide monitoring and early warning.
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Zheng-Yi Feng |
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Zheng-Yi Feng Bo-siang Lin 林博翔 |
author |
Bo-siang Lin 林博翔 |
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Bo-siang Lin 林博翔 Characteristics of seismic signal and self-potentialof slope failure |
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Bo-siang Lin |
title |
Characteristics of seismic signal and self-potentialof slope failure |
title_short |
Characteristics of seismic signal and self-potentialof slope failure |
title_full |
Characteristics of seismic signal and self-potentialof slope failure |
title_fullStr |
Characteristics of seismic signal and self-potentialof slope failure |
title_full_unstemmed |
Characteristics of seismic signal and self-potentialof slope failure |
title_sort |
characteristics of seismic signal and self-potentialof slope failure |
publishDate |
2015 |
url |
http://ndltd.ncl.edu.tw/handle/61980213290715648347 |
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