ISSN 1000-3665 CN 11-2202/P

    真三轴条件下裂隙性黄土力学特性分析

    Experimental Study on Mechanical Properties of Fissured Loess Under True Triaxial Conditions

    • 摘要: 裂隙性黄土是造成黄土高原地区出现地质灾害问题的重要因素之一,探究真三轴条件下裂隙性黄土力学特性演化规律及变形发展对黄土高原地区灾害防治及工程施工安全具有重要意义。为研究真三轴状态下裂隙性黄土力学特性演化规律,本文通过对含有不同裂隙角度的裂隙性黄土开展真三轴试验,分析裂隙性黄土在不同围压及不同b值下力学特性变化规律。结果表明:(1)黄土试样轴向应力峰值随裂隙角度增大表现为:逐渐增大、先减后增和逐渐减小三种不同发展方式。(2)在100 kPa围压b=0.50、0.75与1.00以及200 kPa围压b=0与0.25条件下90°裂隙试样轴向应力-应变曲线出现拐点现象。(3)不同裂隙角度的黄土试样中主应变随大主应变发展可分为剪缩发展、稳定发展和剪胀发展三个发展阶段,同时随着围压增大剪胀阶段明显缩短。(4)裂隙角度相同,b值较小时,随广义剪应力增大,中主应变呈剪胀现象,且裂隙角度越大剪胀越明显。研究结果可为裂隙性黄土工程灾害防治与稳定性评价提供参考。

       

      Abstract: Fissured loess is one of the important factors causing geological disasters in the Loess Plateau region. Exploring the evolution law of mechanical properties and deformation development of fissured loess under true triaxial conditions is of great significance for disaster prevention and control and engineering construction safety in the Loess Plateau region. To study the evolution law of mechanical properties of fissured loess under true triaxial conditions, this paper conducts true triaxial tests on fissured loess with different fissure angles and analyzes the variation law of mechanical properties of fissured loess under different confining pressures and different b values. The results show that: (1) The peak axial stress of loess specimens with different fissure angles shows three different development patterns: gradually increasing, first decreasing and then increasing, and gradually decreasing. (2) Under confining pressures of 100 kPa with b=0.50, 0.75 and 1.00, and 200 kPa with b=0 and 0.25, the axial stress-strain curves of 90° fissured specimens show inflection points. (3) The principal strains of loess specimens with different fissure angles can be divided into three development stages: shear contraction development, stable development and shear expansion development with the development of the major principal strain. At the same time, the shear expansion stage becomes shorter with the increase of confining pressure. (4) When the fissure angles are the same and b values are small, with the increase of generalized shear stress, the intermediate principal strain shows a shear expansion phenomenon, and the larger the fissure angle, the more obvious the shear expansion. The research results can provide a reference for the prevention and control of engineering disasters and stability evaluation of fissured loess.

       

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