海相软土无侧限抗压强度曲线类型分类及影响因素

    CLASSIFICATION OF UNCONFINED COMPRESSIVE STRENGTH CURVE TYPES AND INFLUENCING FACTORS OF MARINE SOFT SOILS

    • 摘要: 无侧限抗压强度是岩土设计中的一种代表性强度。基于连云港地区186组海相软土无侧限抗压强度试验(UTC),对其应力-应变曲线类型进行了分类统计,探讨了影响应力-应变曲线的因素。研究结果表明:应力-应变曲线类型可以归为3个类型。Ⅰ类曲线为软化型,具有明显的轴向应力峰值,Ⅰ类曲线数量占比27%;Ⅱ类曲线为稳定性,不具有明显的峰值,一般应变大于15%后轴向应力才趋向一个定值,Ⅱ类曲线数量占比35%;Ⅲ类曲线为应变硬化型,应变大于20%时轴向应力还没有收敛趋势,Ⅲ类曲线数量占比38%。振动可以促使应力-应变曲线类型由Ⅰ型逐渐转化为Ⅲ型,且破坏应变随着振动时长的增加而变大,无侧限抗压强度数值逐渐减小。取样器类型也对曲线类型有显著影响,Ⅰ类曲线中采用薄壁获取样品的占比90%,厚壁获取样品仅占比10%。K0固结预处理可以恢复土体地应力,促使曲线类型由Ⅱ、Ⅲ型转化为Ⅰ型,获取的抗剪强度接近原位试验获取的土体抗剪强度,且随着取样深度的增加,进行土体应力恢复效果越明显。

       

      Abstract: The unconfined compressive strength is a representative strength in geotechnical design. Based on 186 sets of unconfined compression test(UTC) of marine soft soils in Lianyungang area,the stress-strain curve types were classified and statistically discussed,and the factors affecting the stress-strain curve were discussed. The results showed that the stress-strain curve types can be categorized into three types. Type Ⅰ curves are softening type,with obvious peak axial stress,and the number of type Ⅰ curves accounts for 27%; Type Ⅱ curves are stable,without obvious peak,and the axial stress generally converges to a constant value only after the strain is greater than 15%. The number of Type Ⅱ curves accounts for 35%; Type Ⅲ curves are strain-hardening type. When the strain is greater than 20%,the axial stress has not yet converged,and the number of type Ⅲ curves accounts for 38%. Vibration can lead to the gradual transformation of the stress-strain curve type from type Ⅰ to type Ⅲ,and the damage strain becomes larger with the increase of vibration duration,and the value of unconfined compressive strength gradually decreases. The type of sampler also has a significant effect on the curve type. 90% of the type Ⅰ curves are obtained by thin-walled samples,and only 10% of the type Ⅰ curves are obtained by the thick-walled samples. K0 consolidation pretreatment can restore the soil ground stress and promote the curve type to be transformed from type Ⅱ and Ⅲ to type Ⅰ. The obtained shear strength is close to the soil shear strength obtained from the in-situ test,and the more obvious the soil stress recovery effect is carried out with the increase of sampling depth.

       

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