兰州理工大学学报 ›› 2023, Vol. 49 ›› Issue (3): 109-114.

• 建筑科学 • 上一篇    下一篇

多年冻土区不同深度原状土的力学试验研究

毕贵权*1,*, 熊猛1,2, 柴明堂2, 胡阳1,2, 虞洪1,2   

  1. 1.兰州理工大学 土木工程学院, 甘肃 兰州 730050;
    2.中国科学院西北生态环境资源研究院 冻土国家重点试验室, 甘肃 兰州 730000
  • 收稿日期:2019-08-31 出版日期:2023-06-28 发布日期:2023-07-07
  • 通讯作者: 毕贵权(1979-),男,吉林九台人,博士,副教授. Email:13893692642@163.com
  • 基金资助:
    国家自然科学基金(51568043),冻土工程国家重点实验室年开放基金项目(SKLFSE201008)

Experimental study on mechanical properties of undisturbed frozen soil on different depths in permafrost region

BI Gui-quan1, XIONG Meng1,2, CHAI Ming-tang2, HU Yang1,2, YU Hong1,2   

  1. 1. School of Civil Engineering, Lanzhou Univ. of Tech., Lanzhou 730050, China;
    2. State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
  • Received:2019-08-31 Online:2023-06-28 Published:2023-07-07

摘要: 为探讨多年冻土原状样承受竖向外荷载时的强度和变形特性,对不同深度的原状冻土样进行单轴试验和固结试验,并分析了冻土抗压强度、弹性模量、破坏形态、融沉特性.试验表明:在单轴试验中,浅层土的应力-应变曲线为不规则的非线性曲线,深土层的应力-应变曲线为抛物线形式曲线,随着含冰量的增加以及含砂量的减少,荷载由土颗粒骨架发展为冰晶体承担,抗压强度和弹性模量随深度的增加先减小后增大.冻土的破坏分为三种:延性破坏时外部无明显裂痕,仅产生挤压变形;弱面剪切破坏引起侧向裂缝以及侧向挤压变形;轴向分裂破坏的裂痕从中间至轴向展开.在固结试验中,主固结一般发生在前100 min,深层土的固结应变及融沉系数比浅土层大,且深土层融沉系数受荷载影响较大.

关键词: 抗压强度, 破坏形态, 弹性模量, 融沉系数, 压缩系数

Abstract: In order to investigate the strength and deformation characteristics of the undisturbed sample of permafrost under vertical and outward loading, uniaxial tests and consolidation tests were performed on undisturbed samples of permafrost with different depths to analyze the compressive strength, Elastic Modulus, failure pattern, and thawing characteristics of frozen soil. The test shows that the stress-strain curve of the shallow soil is an irregular nonlinear curve and the stress-strain curve of the deep soil is a parabolic curve in the uniaxial test. As the ice content increases and the sand content decreases, the bearing body of load is developed from the soil particle skeleton to ice crystals, and the compression strength and elastic modulus decrease first and then increase with the increase of soil depth. Failure of frozen soil is divided into three types: there are no obvious cracks on the outside when ductile failure occurs, and only compression deformation occurs; shear failure on the weak surface leads to the lateral cracks and lateral compression deformation; cracks of brittle failure expand from the middle part to the axis. In the consolidation test, the main consolidation generally occurred in the first 100 minutes; the consolidation strain and thawing coefficient of the deep soil are larger than those of the shallow soil layer and the deep soil layer thawing settlement coefficient is greatly affected by the load.

Key words: compressive strength, failure shape, elastic modulus, melting settlement coefficient, compression coefficient

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