冻融过程对高寒区渠道基土力学特性的影响

    Effect of freezing-thawing process on the mechanical properties of canal foundation soils in cold regions

    • 摘要: 高寒区复杂的环境场是渠道基土劣化的重要原因,并由此诱发渠系工程的灾变。开展了湿干循环及湿干冻融耦合循环下膨胀性渠道基土的三轴固结排水剪切试验,描述了渠道基土的应力-应变关系、弹性模量、破坏强度和抗剪强度指标的变化特征,探讨了湿干冻融耦合循环中的冻融过程对渠道基土力学特性的影响。结果表明:湿干循环和湿干冻融耦合循环次数的增长使得渠道基土的应力-应变关系由一般硬化型往弱硬化型(弱软化型)发展,湿干冻融耦合循环过程中的冻融过程加剧了这一转变的发展。同时,湿干冻融耦合循环中的冻融过程易造成渠道基土的弹性模量、破坏强度、黏聚力在耦合循环初期大幅下降,而这一影响随着湿干冻融耦合循环次数的增长逐渐弱化。7次湿干循环后,试样的弹性模量、破坏强度、黏聚力和内摩擦角分别衰减了约13.1%~33.3%、21.2%~27.6%、39.1%和15.6%,低于7次湿干冻融耦合循环后22.3%~34.5%、22.2%~30.9%、44.0%、11.7%的衰减幅度,表明湿干冻融耦合循环中的冻融过程加剧了渠道基土力学性能的衰减,但对试样内摩擦角影响较小。另外,湿干冻融耦合循环中的冻融过程造成低围压下的渠道基土损伤较为明显,以传统弹性模量形式表征渠道基土的损伤度在在一定程度上低估了湿干循环及湿干冻融耦合循环过程对于渠道土体的损伤程度,在高寒区膨胀土渠系工程相关计算与分析中,还应充分考虑渠道土体的破坏强度衰减。研究成果可为北疆供水工程的建设与维护提供一定科学依据。

       

      Abstract: Abstract: Complex environment field in high and cold regions is an important factor for the deterioration of foundation soils, particularly leading to the serious damage of expansive soil canals. Therefore, this study aims to explore the effects of the freezing-thawing process among coupled wetting-drying-freezing-thawing cycles on the mechanical properties of canal foundation soils in cold regions. The expansive soil was also taken from the construction field in Northern Xinjiang, China. Firstly, the coupled wetting-drying-freezing-thawing and cyclic wetting-drying were performed on the expansive soils. A tri-axial consolidation drained shear test was then conducted below the canal structures. The variation characteristics were determined, including the stress-strain relationship, elastic modulus, failure strength, cohesion, and internal friction angel angle of expansive soils below the canal structures in the wetting-drying, and coupled wetting-drying-freezing-thawing cycles. The test results showed that the stress-strain relationship of expansive soils below the canal structures presented from general to weak hardening type (weak softening type), as the increase of wetting-drying and coupled wetting-drying-freezing-thawing cycles. It infers that the freezing-thawing in the coupled wetting-drying-freezing-thawing cycles significantly accelerated the development of transformation. Meanwhile, there was a significant decrease in the elastic modulus, failure strength, and cohesion of expansive soils below the canal structures at the beginning of coupled wetting-drying-freezing-thawing cycles. The decreasing trend was then gradually weakened, with the increase of cycles. Specifically, the elastic modulus, failure strength, cohesion, and internal friction angle of expansive soils below the canal structures decreased by about 13.1%-33.3, 21.2%-27.6,% 39.1%, and 15.6%, respectively, after 7 wetting-drying cycles, lower than the attenuation amplitude of 22.3%-34.5%, 22.2%-30.9%, 44.0%, and 11.7%, respectively, after 7 coupled wetting-drying-freezing-thawing cycles. It indicated that the freezing-thawing strengthen the attenuation of mechanical properties of expansive soils below the canal structures, but there was little effect on the internal friction angle. In addition, there was much more obvious damage of expansive soil under a low confining pressure. Since the damage was normally characterized by the traditional parameter of elastic modulus, there was an underestimated damage level of expansive soils below the canal structures subjected to wetting-drying and coupled wetting-drying-freezing-thawing cycles. As a result, a suggestion was made to consider the failure strength attenuation of expansive soils below the canal structures in high and cold regions. The findings can provide a sound scientific basis for the construction and maintenance of water delivery projects in Northern Xinjiang, China.

       

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