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硅酸盐通报 ›› 2025, Vol. 44 ›› Issue (3): 1170-1181.

• 道路材料 • 上一篇    下一篇

干燥环境下膨润土-纤维改良固化土的裂隙发育特征和强度劣化机理研究

陈建华, 戴自立   

  1. 上海大学力学与工程科学学院,上海 200444
  • 收稿日期:2024-09-11 修订日期:2024-10-19 出版日期:2025-03-15 发布日期:2025-04-01
  • 通信作者: 戴自立,博士,副教授。E-mail:zilidai@shu.edu.cn
  • 作者简介:陈建华(1997—),男,硕士研究生。主要从事流态固化土的研究。E-mail:chenjianhua@shu.edu.cn
  • 基金资助:
    国家自然科学基金(42102318,42472332)

Crack Evolution Characteristic and Strength Deterioration Mechanism of Bentonite-Fiber Improved Solidified Soil in Dry Environments

CHEN Jianhua, DAI Zili   

  1. School of Mechanics and Engineering Science, Shanghai University, Shanghai 200444, China
  • Received:2024-09-11 Revised:2024-10-19 Published:2025-03-15 Online:2025-04-01

摘要: 为研究固化土在干燥环境下的耐久性,本文利用膨润土和玻璃纤维对水泥固化土进行改良,并研究固化土在干燥环境下的裂隙发育特征和强度劣化情况,分析膨润土掺量和纤维掺量对固化土裂隙指标和无侧限抗压强度的影响规律,并借助扫描电子显微镜研究固化土的微观结构劣化机理。结果表明,在固化土中加入膨润土和纤维可明显改善固化土在干燥环境下的耐久性。当膨润土含量为6%(质量分数)、纤维含量为0.3%(质量分数)时,对固化土改良效果最佳。养护龄期为28 d的试件在干燥试验后的无侧限抗压强度折损率仅为3.6%,应力峰值后仍有较高的残余强度,且试件表面没有出现明显裂隙。干燥环境水分蒸发导致试件孔隙率和孔隙体积增大,水化产物分解,从而造成试件开裂,强度劣化。

关键词: 固化土, 膨润土, 玻璃纤维, 干燥环境, 裂隙演化, 强度劣化

Abstract: In order to study the durability of solidified soil in dry environment, bentonite and glass fiber were used to improve the cement solidified soil, and the crack evolution characteristics and strength deterioration of solidified soil in dry environment were studied. The influences of bentonite content and fiber content on crack index and unconfined compressive strength of solidified soil were analyzed, and the microstructure degradation mechanism of solidified soil was studied by scanning electron microscope. The results show that the addition of bentonite and fiber to solidified soil can significantly improve the durability of solidified soil in dry environment. When the bentonite content is 6% (mass fraction) and the fiber content is 0.3% (mass fraction), the improvement effect of solidified soil is the best. The unconfined compressive strength loss rate of specimen with curing age of 28 d after drying test is only 3.6%, and there is still a high residual strength after the peak stress, and there is no obvious crack on the surface of specimen. The evaporation of water in dry environment leads to the increase of porosity and pore volume of specimen, and the decomposition of hydration products, resulting in cracking and strength deterioration of specimen.

Key words: solidified soil, bentonite, glass fiber, dry environment, crack evolution, strength deterioration

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