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  2. College of Bioresources and Agriculture / 生物資源暨農學院
  3. Bioenvironmental Systems Engineering / 生物環境系統工程學系
  4. 行政院國家科學委員會專題研究計畫成果報告:水文對坡地災害因子潛勢影響分析─總計畫暨子計畫:因地震導致孔隙水壓上升對邊坡崩壞之影響(III)
 
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行政院國家科學委員會專題研究計畫成果報告:水文對坡地災害因子潛勢影響分析─總計畫暨子計畫:因地震導致孔隙水壓上升對邊坡崩壞之影響(III)

Date Issued
2004
2004-07-31
Date
2004
2004-07-31
Author(s)
譚義績  
DOI
922625Z002031
URI
http://ntur.lib.ntu.edu.tw//handle/246246/10780
Abstract
Under soil slope influenced by earthquake or vegetation root system, the characteristics of soil material and movement of soil water content is quite important. The pores of soil will be deformed by the earthquake. Soil shear strength and soil characteristics will produce changes with the hydrological processes (wetting or drying). In order to accurate calculation slope factor of safety, we must consider changes in the environment of variation pores of soil, vegetation root system and hydrological processes (wetting or drying). This root force model based on Wu of research, in addition, Bishop and Janbu model and unsaturated slope factor of safety derived by myself carry on the safe factor analysis of different slope. The selection of vegetation is Taiwan China fir and mountain jute, and probe into safety factor of unsaturated soil slope due to different the depth of wetting front, different slope and root force model. This research shows that safety factor of vegetation slope is a bit higher than without safety factor of vegetation slope in the same slope. But the unsaturated slope factor of safety derived by myself is obviously different from Bishop and Janbu’s model with the depth of wetting front.
Subjects
Soil shear strength
slope factor of safety
wetting front
Publisher
臺北市:國立臺灣大學生物環境系統工程學系暨研究所
Type
report
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922625Z002031.pdf

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