基于动三轴试验的花岗岩残积土结构性与动态力学特性研究

    Structural characteristics and dynamic mechanical properties of granite residual soil based on dynamic triaxial tests

    • 摘要: 花岗岩残积土是华南沿海及其他多雨地区广泛分布的一种典型土壤,因其特殊的地质成因,兼具较高强度和较大孔隙比的特点,在地下工程建设中广泛应用。通过动三轴试验系统研究了花岗岩残积土在不同土样状态(原状样、重塑样、饱和样)下的动态力学特性。试验结果表明,花岗岩残积土的动态响应显著受其结构性和外部荷载条件影响。在小振次和低动应力幅值条件下,原状样因其天然结构性表现出较强的抗变形能力,但在高动应力幅值和高振次作用下,其结构性逐渐破坏,动应变显著增大并可能超过重塑样。此外,动应变0.25%可作为花岗岩残积土刚度变化的临界值,在此值以下试样刚度较高,超出该值后刚度显著衰减。动剪切模量与动应变的关系曲线表现出非线性特性,滞回圈和动骨干曲线可通过Hardin-Drnevich动本构模型较好拟合,但在低动应力原状样的拟合效果略显不足。研究成果可为复杂工程条件下花岗岩残积土的性能预测与设计优化提供参考。

       

      Abstract: The granite residual soil is a typical soil widely distributed in the coastal areas of South China and other rainy regions. Due to its unique geological formation, it exhibits both high strength and large porosity, making it widely used in underground engineering. The dynamic mechanical properties of granite residual soil in different sample states (undisturbed, remolded, and saturated) are investigated through the dynamic triaxial tests. The results indicate that the dynamic response of the granite residual soil is significantly influenced by its structural characteristics and external loading conditions. Under low cyclic loading and small dynamic stress amplitudes, the undisturbed samples demonstrate strong resistance to deformation due to their natural structure. However, at higher dynamic stress amplitudes and cyclic loading, their structural integrity is gradually destroyed, leading to significantly increased dynamic strain, even exceeding that of the remolded samples. The dynamic strain of 0.25% is identified as the critical threshold for stiffness degradation in the granite residual soil, and below this value, the samples exhibit high stiffness, while the stiffness decreases markedly beyond this threshold. The relationship between dynamic shear modulus and dynamic strain exhibits nonlinear behavior. The hysteresis loops and dynamic backbone curves are well-fitted using the Hardin-Drnevich (H-D) constitutive model, though the model shows some limitations for the intact samples under low dynamic stress. These findings provide valuable insights for predicting and optimizing the performance of the granite residual soil under complex engineering conditions.

       

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