干湿循环下川中红层泥岩力学特性劣化机制和能量演化特征试验研究

    EXPERIMENTAL STUDY ON DETERIORATION MECHANISM OF MECHANICAL PROPERTIES AND ENERGY EVOLUTION OF RED MUDSTONE UNDER DRY-WET CYCLE IN CENTRAL SICHUAN

    • 摘要: 地基平顺是高铁列车安全运营的保障。为探究川中红层地区高铁红层泥岩地基不均匀变形机制,开展了不同干湿循环次数下红层泥岩单轴压缩试验和单轴循环加卸载试验,结合场发射扫描电镜技术(FESEM)测试结果,从能量耗散理论角度,分析了干湿循环次数对红层泥岩力学强度劣化的影响规律及机制。研究结果表明:随干湿循环次数的增多,红层泥岩完整性系数、力学性能强度均出现劣化,其中前5次干湿循环时强度劣化速度较快,5次干湿循环后强度呈缓慢持续下降趋势;干湿循环会导致红层泥岩微观结构松散,孔隙数量增加,其中小孔(0~0.5 μm)数量在5次干湿循环后趋于稳定,中孔(0.5~1 μm)和大孔(> 1 μm)依旧呈缓慢上升趋势;干湿循环会导致红层泥岩受压过程中的弹性应变能和耗散能下降,其中前5次干湿循环破碎耗能快速下降,5次干湿循环后,破碎耗能缓慢增加;摩擦耗能在0~1次干湿循环时呈快速下降趋势,1~8次干湿循环时缓慢降低,8~10次干湿循环上升速率较缓。多次干湿循环会导致红层泥岩的微观结构特征出现持续性改变,影响其在受到外部荷载扰动时能量演化特征,使其力学性能持续劣化。

       

      Abstract: Foundation stability,one of the most important factors in high-speed railways,is influenced by uneven deformation in red layer areas. In order to investigate the uneven deformation mechanism of high-speed railway foundations in the red layer area of central Sichuan,this paper conducted uniaxial compression tests and uniaxial cyclic loading-unloading tests on red mudstone under different dry-wet cycles. Then,combined with the test results of field emission scanning electron microscopy(FESEM),the deterioration law and mechanism of the mechanical strength of red mudstone under dry-wet cycles were analyzed based on energy dissipation theory. The results show that with the increase in the number of dry-wet cycles,the integrity coefficient and strength of the red mudstone decrease. Among these changes,the strength degradation is faster in the first five dry-wet cycles and then slows down but continues to decline after the fifth dry-wet cycle. During these dry-wet cycles,an increase in pores and loosening of the microstructure occur in the red mudstone. In detail,the number of small pores(0~0.5 μm) tends to stabilize after five dry-wet cycles,while the number of medium(0.5~1 μm) and large pores(> 1 μm) shows a slow upward trend. These changes lead to a decrease in both elastic strain energy and dissipation energy during the compression process of red mudstone under dry-wet cycles. Specifically,breakage energy dissipation decreases rapidly after the first five dry-wet cycles and increases slowly after the fifth dry-wet cycle. Meanwhile,friction energy dissipation shows a rapid decrease after the first dry-wet cycle,then a gradual decrease during the 1st-8th dry-wet cycles,and finally a slow increase in the last two cycles. Red mudstone undergoes continuous changes in microstructural characteristics under multiple dry-wet cycles. When disturbed by external loads,its energy evolution characteristics are affected,further deteriorating its mechanical properties continuously.

       

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