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许健, 张明辉, 李彦锋, 武智鹏. Na2SO4盐渍原状黄土冻融过程劣化特性试验研究[J]. 岩土工程学报, 2020, 42(9): 1642-1650. DOI: 10.11779/CJGE202009008
引用本文: 许健, 张明辉, 李彦锋, 武智鹏. Na2SO4盐渍原状黄土冻融过程劣化特性试验研究[J]. 岩土工程学报, 2020, 42(9): 1642-1650. DOI: 10.11779/CJGE202009008
XU Jian, ZHANG Ming-hui, LI Yan-feng, WU Zhi-peng. Experimental study on deterioration behavior of saline undisturbed loess with sodium sulphate under freeze-thaw action[J]. Chinese Journal of Geotechnical Engineering, 2020, 42(9): 1642-1650. DOI: 10.11779/CJGE202009008
Citation: XU Jian, ZHANG Ming-hui, LI Yan-feng, WU Zhi-peng. Experimental study on deterioration behavior of saline undisturbed loess with sodium sulphate under freeze-thaw action[J]. Chinese Journal of Geotechnical Engineering, 2020, 42(9): 1642-1650. DOI: 10.11779/CJGE202009008

Na2SO4盐渍原状黄土冻融过程劣化特性试验研究

Experimental study on deterioration behavior of saline undisturbed loess with sodium sulphate under freeze-thaw action

  • 摘要: 选取西安Q3原状黄土,人工制备不同Na2SO4含量的盐渍原状黄土试样。通过冻融作用下的三轴剪切及CT扫描试验,研究了Na2SO4盐渍原状黄土冻融过程劣化规律及微细观结构损伤演化机制。结果表明:冻融作用对应力–应变曲线的类型及特征无明显影响,均表现为应变硬化型。破坏偏应力随冻融次数增加逐渐减小,但衰减速率逐渐减小,表现出减速劣化特征;冻融条件下破坏偏应力随着含盐量增加逐渐减小,且表现出线性或加速劣化特征。黏聚力呈现与破坏偏应力相似的劣化特征;内摩擦角变化幅值较小且无明显规律。冻融与盐蚀劣化因子的比值随冻融次数增加逐渐增大但增速逐渐减小,随含盐量增大逐渐减小且衰减速率逐渐减小。CT数ME值呈现与破坏偏应力和黏聚力相似的劣化规律;构建了CT细观损伤变量演化方程,可较好预测试样冻融过程细观结构损伤演化规律。宏细观损伤变量表现出一致的变化规律,表明CT细观结构损伤变量准确揭示了宏观三轴剪切强度指标的劣化机理。

     

    Abstract: Xi'an Q3 undisturbed loess was chosen to artificially prepare saline undisturbed loess specimens with different gradients of sodium sulphate content. The triaxial shear and CT scanning tests under freeze-thaw action are then conducted to study deterioration behavior and damage mechanism of microstructure of the saline undisturbed loess with sodium sulphate. The results show that the freeze-thaw action has no obvious effect on the type of stress-strain curves, which constantly present characteristics of strain hardening. The failure deviator stress decreases with the increasing number of freeze-thaw cycles while the attenuation rate gradually declines, indicating that freeze-thaw action results in weakening deterioration rate. Moreover, the failure deviator stress experiences a linear or growing decline rate at higher salt content, demonstrating that salt erosion leads to linear or strengthening deterioration rate. The cohesion exhibits the similar characteristics of deterioration with the failure deviator stress. The internal friction angle shows a little variation and no explicit regularity. The ratio of freeze-thaw deterioration factor to that for salt erosion increases with a growing number of freeze-thaw cycles, while its growth rate declines. In addition, the ratio decreases with higher salt content and its attenuation rate also declines. The ME value of CT scanning presents the similar variation with failure deviator stress and cohesion. A formula for microscopic damage variable is then established, and can well predict the damage rules of microstructure of specimens under freeze-thaw action. Both the macroscopic and microscopic damage variables show the consistent variation, indicating that microscopic damage variable well reveals the deterioration mechanism of triaxial shear strength indexes.

     

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