研究生: |
劉信良 Sin-Liang LIOU |
---|---|
論文名稱: |
複合式非破壞檢測於類岩斜剪過程之巨微觀破壞演化 Coupled Nondestructive Techniques to Study the Macro and Micro Fracture Behavior of Rock-like Material under Inclined Shear Tests |
指導教授: |
陳堯中
Yao-Chung Chen |
口試委員: |
陳立憲
none 陳志南 none |
學位類別: |
碩士 Master |
系所名稱: |
工程學院 - 營建工程系 Department of Civil and Construction Engineering |
論文出版年: | 2008 |
畢業學年度: | 96 |
語文別: | 中文 |
論文頁數: | 117 |
中文關鍵詞: | 初裂時機 、石膏 、斜向剪切試驗 、聲射技術 、電子斑紋干涉術 |
外文關鍵詞: | electronic speckle pattern interferometry (ESPI), acoustic emission (AE), inclined shear test, gypsum, crack initiation. |
相關次數: | 點閱:382 下載:4 |
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本研究以電子斑紋干涉術(Electronic Speckle Pattern Interferometry, ESPI)為主,輔以聲射技術(Acoustic Emission, AE),針對岩石最常發生之剪力破壞模式,進行一系列探討。為了搭配電子斑紋干涉術及聲射技術,建置一套斜向剪切試驗系統,以斜向剪切試驗模擬岩石受力行為,實驗中採用石膏及石膏砂漿作為人造類岩材料。
本研究分成四大主軸:(a)斜向剪切儀之適用性(b)顆粒材料之膨脹角求算。(c)相同試體尺寸下其顆粒有無對於剪力破壞模式之差別性。(d)以電子斑紋干涉術量測石膏材料之初裂時機。
由斜向剪切儀與傳統直接剪力儀之試驗結果比對得知,在正向應力約4 MPa以下,兩者所得之巨觀強度相當接近,驗證斜向剪切儀之適用性。
經斜向剪切試驗結果可得知石膏砂漿試體之膨脹角約為11°,而當正向應力減少時,其破壞模式會由張力破壞趨近於剪力破壞,其結果與數值軟體分析頗為相似,而使用ESPI系統觀察到相同材料其初裂時機略為相同,石膏砂漿試體初裂時機約為加載百分比82∼86%之間,並結合AE系統可得知試體由內部微裂縫之發展趨勢。
耦合電子班紋干涉術與聲射技術,可得知材料微觀裂縫之衍化,更能瞭解剪力破壞之機理,研究成果可供工程實務之佐參。
This research investigated the mechanism of shear failure by performing a series of tests together with measurements of ESPI and AE. To couple the nondestructive technique of ESPI and AE, a set of inclined shear test equipment was designed and built. Gypsum and gypsum-sand mixture were used to prepare the specimens.
Four major topics were investigated in this research: (1) the correctness and suitability of the inclined shear device, (2) the dilatancy angle of the specimen, (3) the influence of particle size on the shear failure mode, (4) the timing of crack initiation investigated by ESPI.
By comparisons of the results of inclined shear tests with direct shear tests, it is shown that both tests give similar strength parameters under the condition of normal stress less than 4MPa. The correctness and suitability of the inclined shear device was approved.
The dilatancy angle is about 11 degrees for specimen of gypsum-sand mixture. The failure mode evolved from tension to shear failure as the normal stress decreased. Similar behavior was also observed from the results of numerical analysis. The crack initiation, observed by ESPI, occurred at about the same loading level for same material. For gypsum-sand mixture, the crack initiation occurred at about 82~86% loading level. The development and evolution of microcracks of the specimens could be studied by AE technique.
By coupling the nondestructive technique of ESPI and AE, the evolution of microcracks and the mechanism of shear failure could be studied more thoroughly, and the results could be referred to the construction practice.
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