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基于原位蠕變試驗的滑帶土特性研究及應(yīng)用 ——以三峽庫區(qū)黃土坡滑坡為例

發(fā)布時間:2021-02-11 10:46
  滑坡災(zāi)害是影響人類生命與財產(chǎn)安全的重大地質(zhì)災(zāi)害之一,而在我國的三峽庫區(qū)其發(fā)生尤為頻繁。因此,對滑坡變形的機理展開深入研究具有重要的實際意義。一般而言,分析滑坡的穩(wěn)定性是通過現(xiàn)場取樣、室內(nèi)或原位試驗(直剪、三軸等)的手段獲得巖土體的抗剪強度參數(shù),從而進一步計算得到滑坡的安全系數(shù)。由于場地條件的限制,開展原位試驗通常只能針對滑體部分進行,而無法對滑帶部分進行有效的測試;瑤强刂苹聠右约斑\動過程的關(guān)鍵結(jié)構(gòu),其結(jié)構(gòu)與強度通常與滑體有較大差異;因此,對滑帶開展原位試驗理論上可以反映出更為真實的滑坡穩(wěn)定性狀態(tài)。目前,蠕變試驗是研究巖土體長期變形與強度性質(zhì)的唯一途徑。對于尚未發(fā)生或正在經(jīng)歷緩慢變形的滑坡而言,開展原位蠕變試驗?zāi)軌蛘鎸嵙私饣瑤恋淖冃翁匦?從而對滑坡穩(wěn)定性評價與預(yù)測提供更加合理的依據(jù)。黃土坡滑坡是三峽庫區(qū)已探明的最大規(guī);,根據(jù)監(jiān)測數(shù)據(jù)可知,該滑坡長期處于緩慢變形過程(滑坡前部地表位移約30 mm/年);滑帶的埋深深度約50-70 m,由于長期上部荷載的影響,滑帶結(jié)構(gòu)致密,與重塑樣有明顯區(qū)別。基于上述特征,本文針對黃土坡1號滑坡(黃土坡滑坡變形最大的子滑坡)的滑帶土開展了原位蠕... 

【文章來源】:中國地質(zhì)大學(xué)湖北省 211工程院校 教育部直屬院校

【文章頁數(shù)】:119 頁

【學(xué)位級別】:博士

【文章目錄】:
作者簡歷
摘要
ABSTRACT
Chapter 1 Introduction
    1.1 Research background and significance
    1.2 Overviews on present research
        1.2.1 Latest achievements on acquiring shear strength of the sliding zone soil
        1.2.2 Research on the creep properties of sliding zone soil
    1.3 Existing shortcomings
    1.4 Research method
        1.4.1 Research contents
        1.4.2 Innovative points
        1.4.3 Technology roadmap
Chapter 2 The Huangtupo landslide
    2.1 Regional geological conditions of the Huangtupo landslide area
        2.1.1 Overview of The Huangtupo Landslide
        2.1.2 Topography and Landform
        2.1.3 Strata and lithology
        2.1.4 Geological structure
        2.1.5 Hydrogeological conditions
    2.2 Materials and structures by investigations
        2.2.1 The No.1 landslide
        2.2.2 The No.2 landslide
        2.2.3 The Substation landslide
        2.2.4 The Garden spot landslide
    2.3 Deformation monitoring of the landslide
        2.3.1 GPS monitoring
        2.3.2 Inclinometer monitoring
        2.3.3 TDR monitoring on deep deformation
        2.3.4 Monitoring of crack deformation
    2.4 Summary of this chapter
Chapter 3 In situ triaxial creep test on sliding zone soil
    3.1 Significance of the in situ triaxial creep test
    3.2 Instrument used for in situ triaxial testing
    3.3 Loading scheme and test result
    3.4 Analysis on the low compressibility of the sample
        3.4.1 High preexisting compression degree
        3.4.2 High rock content
    3.5 Constitutive law
        3.5.1 Elements for the constitutive equation
        3.5.2 Linear viscoplasticity term
        3.5.3 Nonlinear viscoplasticity term
    3.6 Anisotropic deformation
    3.7 Landslide movement related to the sample
    3.8 Summary of this chapter
Chapter 4 Shear strength and deformative behavior of remoulded sliding zone soil
    4.1 Soil structures
    4.2 Soil compactness
        4.2.1 Soil porosity
        4.2.2 Dry density
        4.2.3 Relative density
    4.3 Structure capacity of tested sliding zone soil
        4.3.1 Capacity from soil structure
        4.3.2 Capacity from soil-water bond
    4.4 Direct shear test demonstrating the structure capacity
        4.4.1 Sampling and preparation
        4.4.2 Test plan
        4.4.3 Results
    4.5 Summary of this chapter
Chapter 5 Case study on the Huangtupo No.1 landslide
    5.1 Ring shear test on the sliding zone soil
        5.1.1 Introduction of the ICL-2 apparatus
        5.1.2 Test process
        5.1.3 Test results
    5.2 Simulations on initiation of the Huangtupo No.1 landslide
        5.2.1 The LS-RAPID
        5.2.2 Shear strength parameters to be input
        5.2.3 Modelling of the Hunagtupo No.1 landslide
        5.2.4 Simulative process and results
        5.2.5 Analysis and conclusion
    5.3 Summary of this chapter
Chapter 6 Conclusions and outlook
    6.1 Conclusions
    6.2 Outlook
Acknowledgements
References


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期刊論文
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博士論文
[1]庫水作用下滑坡流固耦合作用及變形研究[D]. 汪斌.中國地質(zhì)大學(xué) 2007

碩士論文
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