王旭宏, 胡继华, 耿学勇, 杨立建, 李昶. 2015: 吉阳核电厂古近系软岩现场剪切试验及成果分析. 工程地质学报, 23(s1): 745-749. DOI: 10.13544/j.cnki.jeg.2015.s1.114
    引用本文: 王旭宏, 胡继华, 耿学勇, 杨立建, 李昶. 2015: 吉阳核电厂古近系软岩现场剪切试验及成果分析. 工程地质学报, 23(s1): 745-749. DOI: 10.13544/j.cnki.jeg.2015.s1.114
    WANG Xuhong, HU Jihua, GENG Xueyong, YANG Lijian, LI Chang. 2015: FIELD SHEAR TEST AND ANALYSIS OF PALEOGENE SOFT ROCKS IN THE SITE OF JIYANG NUCLEAR POWER PLANT. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 745-749. DOI: 10.13544/j.cnki.jeg.2015.s1.114
    Citation: WANG Xuhong, HU Jihua, GENG Xueyong, YANG Lijian, LI Chang. 2015: FIELD SHEAR TEST AND ANALYSIS OF PALEOGENE SOFT ROCKS IN THE SITE OF JIYANG NUCLEAR POWER PLANT. JOURNAL OF ENGINEERING GEOLOGY, 23(s1): 745-749. DOI: 10.13544/j.cnki.jeg.2015.s1.114

    吉阳核电厂古近系软岩现场剪切试验及成果分析

    FIELD SHEAR TEST AND ANALYSIS OF PALEOGENE SOFT ROCKS IN THE SITE OF JIYANG NUCLEAR POWER PLANT

    • 摘要: 岩土体的强度参数确定一直是岩土力学界的一大难题, 尤其对于某些特殊的软岩。本文通过对吉阳核电软岩地基的现场剪切试验研究, 并结合室内三轴试验对比分析, 阐述了吉阳地区软岩应力-应变的关系, 提出了可靠的岩体强度参数。研究结果表明: (1)水平剪切作用下, 吉阳古近系软岩试样出现了明显塑性变形和应力屈服特征, (2)各试验点的剪切过程基本表现为全应力-应变过程, 包括:线弹性变形段、弹塑性变形段、峰值段及应变软化段, (3)吉阳古近系软岩属塑性破坏岩体, 其变形特征更接近于土体特征, 可利用现场剪切试验的屈服强度确定抗剪强度参数, 即c=19.5kPa, =33.1, (4)现场剪切试验所获取的值与三轴试验成果基本一致, 而c值略低于三轴试验, 考虑到现场剪切试验更能反映场地实际条件, 结果更具代表性。

       

      Abstract: The determination of strength parameters of rock and soil has always been the difficult problem in the geotechnical field, especially for soft rock. The relationship between stress and strain of soft rock is illustrated and reliable strength parameters is presented, by means of in-situ shear test in the soft rock foundation of Jiyang nuclear power plant and combined with laboratory three-axial test. The results show that: (1)Apparent stress yield and plastic deformation exist in the process of horizontal shear of Tertiary soft rock samples; (2)Each in-situ soft rock sample shows complete curves of stress-strain relationship, including linearly elastic part, elastic-plastic part, peak part and strain softening part; (3)Tertiary rock in Jiyang nuclear power plant, whose deformation characteristic is more similar to soil, is rock with plastic failure characteristic and the shear strength parameters can be determined by the yield strength of in-situ shear test, i.e.c=19.535kPa and =33.07; (4) obtained by in-situ shear test is equivalent to that obtained by three-axial test, while c obtained by in-situ shear test is a bit less than that obtained by three-axial test, and the former c and are more representative, considering that in-situ shear test reflects the actual situation better.

       

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