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Undrained brittleness of sand in triaxial compression and ring shear tests

机译:三轴压缩和环剪试验中砂的不排水脆性

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Undrained brittleness index, I_B, is defined as the difference between the peak and critical undrained shear strengths normalized by the peak undrained strength, and indicates soil contractiveness and severity of strain softening. In this study, the results of 25 undrained triaxial compression and 20 constant volume ring shear tests performed on two clean sands and one silty sand are used to evaluate I_B. The results illustrate that I_B increases with initial void ratio and state parameter and is affected by particle shape and particle damage, but is independent of the mode of shear (triaxial compression and ring shear). In addition, I_B appears uniquely related to the ratio of consolidation stress to effective stress at critical state, σ'_c/σ'_(cs), and critical strength ratio, s_u(critical)/σ'_c, independent of sand type, mode of shear, initial fabric, and particle damage. These relationships suggest an upper bound critical strength ratio of about 0.3.
机译:不排水脆性指数I_B定义为峰值和临界不排水剪切强度之间的差,该强度由峰值不排水强度归一化,表示土壤收缩性和应变软化的严重程度。在这项研究中,使用25个不排水的三轴压缩和20个恒容环剪试验的结果对两种清洁砂和一种粉质砂进行了评估,以评估I_B。结果表明,I_B随着初始空隙率和状态参数的增加而增加,并受颗粒形状和颗粒损伤的影响,但与剪切模式(三轴压缩和环剪切)无关。此外,I_B似乎与固结应力与临界状态下的有效应力之比σ'_c/σ'_(cs)和临界强度比s_u(critical)/σ'_c唯一相关,与沙子类型无关,剪切模式,初始织物和颗粒损坏。这些关系表明上限临界强度比约为0.3。

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