岩石節理面幾何變化對剪力強度之影響

碩士 === 國立臺灣大學 === 土木工程學研究所 === 90 === In general, the shear strength of rock joint is affected by the normal force, the mechanical properties of intact rock, and the morphological feature of joint surface. Owing to the different sizes of rock joints, the shear strength of rock joint is also differen...

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Main Author: 鄒岳展
Other Authors: 翁作新
Format: Others
Language:zh-TW
Published: 2002
Online Access:http://ndltd.ncl.edu.tw/handle/46478879975722416150
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spelling ndltd-TW-090NTU000150242015-10-13T14:38:04Z http://ndltd.ncl.edu.tw/handle/46478879975722416150 岩石節理面幾何變化對剪力強度之影響 鄒岳展 碩士 國立臺灣大學 土木工程學研究所 90 In general, the shear strength of rock joint is affected by the normal force, the mechanical properties of intact rock, and the morphological feature of joint surface. Owing to the different sizes of rock joints, the shear strength of rock joint is also different. In this study, we investigate the influence of geometrical variation of rock joint on the shear strength. In order to simulate the irregular rock joint, we use the LOM1015-PLUS system to produce the rapid prototype, and choose the mixture of gypsum and quartz powder as the joint material. We use Barton’s standard profiles of JRC=4~6 and JRC=18~20 and a nature profile of Nan-Gang sandstone to be our irregular joints. In geometrical variation, we choose the divided, enlarged, reduced, and repeated profiles as the joint model. Based on the result of a serial of direct shear tests, we discuss the change of shear strength of rock joints of different specimen sizes by controlling the normal stresses. The following conclusions are drawn:(1) Not every shear strength of smaller divided specimen is higher than the larger one, while as a whole, the average shear strength of the smaller specimens is higher than that of the original profile; (2)When we enlarge the profile proportionally, there is no obvious tendency of change in shear strength at the same normal stress;(3)With increasing the specimen sizes with repeated profiles, the shear strength tends to reduce. When the profiles are smoother, this phenomenon becomes unobservable. 翁作新 2002 學位論文 ; thesis 77 zh-TW
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language zh-TW
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sources NDLTD
description 碩士 === 國立臺灣大學 === 土木工程學研究所 === 90 === In general, the shear strength of rock joint is affected by the normal force, the mechanical properties of intact rock, and the morphological feature of joint surface. Owing to the different sizes of rock joints, the shear strength of rock joint is also different. In this study, we investigate the influence of geometrical variation of rock joint on the shear strength. In order to simulate the irregular rock joint, we use the LOM1015-PLUS system to produce the rapid prototype, and choose the mixture of gypsum and quartz powder as the joint material. We use Barton’s standard profiles of JRC=4~6 and JRC=18~20 and a nature profile of Nan-Gang sandstone to be our irregular joints. In geometrical variation, we choose the divided, enlarged, reduced, and repeated profiles as the joint model. Based on the result of a serial of direct shear tests, we discuss the change of shear strength of rock joints of different specimen sizes by controlling the normal stresses. The following conclusions are drawn:(1) Not every shear strength of smaller divided specimen is higher than the larger one, while as a whole, the average shear strength of the smaller specimens is higher than that of the original profile; (2)When we enlarge the profile proportionally, there is no obvious tendency of change in shear strength at the same normal stress;(3)With increasing the specimen sizes with repeated profiles, the shear strength tends to reduce. When the profiles are smoother, this phenomenon becomes unobservable.
author2 翁作新
author_facet 翁作新
鄒岳展
author 鄒岳展
spellingShingle 鄒岳展
岩石節理面幾何變化對剪力強度之影響
author_sort 鄒岳展
title 岩石節理面幾何變化對剪力強度之影響
title_short 岩石節理面幾何變化對剪力強度之影響
title_full 岩石節理面幾何變化對剪力強度之影響
title_fullStr 岩石節理面幾何變化對剪力強度之影響
title_full_unstemmed 岩石節理面幾何變化對剪力強度之影響
title_sort 岩石節理面幾何變化對剪力強度之影響
publishDate 2002
url http://ndltd.ncl.edu.tw/handle/46478879975722416150
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