土工格栅与砾性土界面特性的拉拔试验研究

    Interface characteristics of geogrid and gravelly soil by pullout tests

    • 摘要: 路基工程中,长期受到上部荷载作用的加筋砾性土填料易发生细粒侵入现象,造成筋土界面力学特性劣化。基于拉拔速率、相对密实度、法向应力等因素,对土工格栅与不同细粒含量的含高塑性细粒砾性土进行拉拔试验,探讨了多因素耦合对筋土界面强度特性与体变特性的影响规律。研究结果表明:在不同拉拔速率下,细粒含量增加会导致拉拔阻力曲线由硬化变为软化,界面剪缩性逐渐增强。中密实度时,细粒含量0%的拉拔阻力曲线由于颗粒分布不均匀出现阶梯式下降。剪缩性在低密实度、高细粒含量时显著。法向应力相同时,细粒含量提高会导致峰值拉拔阻力和位移减少,制约剪胀性。综合摩擦因数比K与法向应力 \sigma _\textv 、细粒含量Fc呈幂函数关系。细粒含量10%为砾性土界限细粒含量,该细粒含量下的土工格栅与砾性土的拉拔界面强度与变形特性发生过渡变化,体变从剪胀向剪缩转化,界面强度逐渐降低。

       

      Abstract: In the field of roadbed engineering, the reinforced gravelly soil filling materials subjected to long-term upper loads are prone to phenomena such as intrusion of fine particles, leading to the deterioration of the mechanical properties at the reinforcement-soil interface. The pullout tests on the geogrid and gravelly soil with different contents of high plastic fine particles are conducted based on the factors such as pull-out rate relative compactness and normal stress. The influence rules of multi-factor coupling on the strength characteristics and volume change characteristics of the reinforced soil interface are discussed. The research findings indicate that under different pulling rates, the increase in fine particle content causes the pullout resistance curve to transition from hardening to softening, with the interfacial shear shrinkage gradually increasing. The particle contact state within the specimen at medium compaction is uneven, and the pull-out resistance curve shows a stepwise decline at content of fine particles the of 0%. The shear shrinkage is significant at low compaction density and high content of fines particles. When the normal stress is the same, an increase in the content of fine particles leads to a reduction in the peak pull-out resistance and displacement, constraining dilatancy. The comprehensive friction factor ratio is in a power function relationship with the normal stress and content of fine particles. The content of fine particles of 10% is the limit one of gravelly soil, and the pullout interface strength and deformation characteristics between geogrid and gravel soil change from dilatancy to shear shrinkage, and the interface strength decreases gradually.

       

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