土工基础 ›› 2024, Vol. 38 ›› Issue (6): 1093-1098.

• 测试技术 • 上一篇    下一篇

干湿、冻融循环作用下黑土力学特性试验研究

卢 正1,2,高士军1,赵名扬2,苏安双1,王 淼1,骆行文2   

  1. (1.黑龙江省水利科学研究院,哈尔滨 150080;2.中国科学院武汉岩土力学研究所,武汉 430071)
  • 收稿日期:2024-03-26 修回日期:2024-05-07 出版日期:2024-12-31 发布日期:2024-12-20
  • 通讯作者: 高士军(1966-),男,教授级高级工程师,研究方向为农田水利及水土保持。
  • 作者简介:卢正(1982-),男,研究员,研究方向岩土力学及岩土工程。
  • 基金资助:
    水利部重大科技项目(SKS-2022095)

Mechanical Properties of Black Soil Under Dry-Wet, Freeze-Thaw Cycles

LU Zheng1,2, GAO Shijun1, ZHAO Mingyang2, SU Anshuang1, WANG Miao1, LUO Xingwen2   

  1. (1.Heilongjiang Province Hydraulic Research Institute, Harbing 150080;
    2.Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan 430071)
  • Received:2024-03-26 Revised:2024-05-07 Online:2024-12-31 Published:2024-12-20

摘要: 为了对比分析干湿、冻融循环下黑土的力学特性,进行了两种循环作用下黑土土样裂隙观测、体应变测量、直剪试验及无侧限压缩试验。试验测试结果表明:①黑土表现为湿胀干缩、冻胀融缩的特性。首次干湿循环后,黑土试样的净体应变为12.5%,产生了明显裂隙;首次冻融循环后,试样的净体应变为0.45%,无明显裂隙。②首次干湿循环后黑土试样内摩擦角减小最快,从25.2°减小到23.7°,经过3次干湿循环后内摩擦角基本稳定。首次冻融循环作用后黑土试样内摩擦角从25.2°减小到23.4°,随后在23.4°附近波动。两种循环作用下,粘聚力均随着循环次数增加而减小,且干湿循环后粘聚力衰减更多。③首次干湿循环后,黑土试样无侧限抗压强度衰减32.3%;首次冻融循环后,无侧限抗压强度衰减38.2%。黑土试样的无侧限抗压强度均在经历3次循环后趋于稳定。

关键词: 黑土, 干湿循环, 冻融循环, 剪切强度, 体应变

Abstract: To analyze the mechanical property changes of the black soil under dry-wet and freeze-thaw cycles, the fissure observation, volumetric strain measurements, direct shear tests and unconfined compression tests are performed on black soil samples under the two cycling modes. The results show that: (1) Black soils are characterized by the wet swelling and the dry shrinkage, the frost swelling and the melt shrinkage. After the first dry-wet cycle, the net volumetric strain is 12.5% and obvious cracks occur; After the first freeze-thaw cycle, the net volumetric strain is 0.45% without obvious cracks. (2) The internal friction angle of black soil samples decreases the most after the first dry-wet cycle, from 25.2° to 23.7°, and is basically stable after the third cycle. The internal friction angle decreases from 25.2° to 23.4° after the first freeze-thaw cycle and then fluctuates around 23.4°. In both cycling modes, the cohesion decreases with the increase of the number of cycles, and the decay of the cohesion is greater after the dry-wet cycles. (3) After the first dry-wet cycle, the unconfined compressive strength of the black soil samples decreases by 32.3%. After the first freeze-thaw cycle, the unconfined compressive strength deceases by 38.2%. The unconfined compressive strength of black soil samples is stabilized in the third cycle.

Key words: Black Soil, Dry-Wet Cycles, Freeze , Thaw Cycles, Shear Strength , Volumetric Strain

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