干湿循环下石灰-纤维改良黄土宏观性能劣化研究

    Degradation of macroscopic properties of lime-fiber modified loess under wetting-drying cycles

    • 摘要: 为探究石灰-纤维改良黄土(灰筋黄土)干湿循环作用下的宏观性能劣化规律,本文通过直剪试验、崩解试验和渗透试验,分析了灰筋黄土抗剪强度、崩解系数以及渗透系数的变化。结果表明:石灰水化生成的胶凝物质可填充纤维加筋形成的孔隙,增强土体密实性,同时抑制渗流通道发展;15次干湿循环后,加筋黄土和灰筋黄土的崩解系数相较于黄土分别增加了6.5%和10.7%,渗透系数分别增加了8.3%和18.2%;灰筋黄土的宏观性能劣化速率随干湿循环次数的增加而逐渐趋缓,采用双曲线模型可反映宏观性能劣化与干湿循环次数的映射关系;灰筋黄土的宏观性能显著优于单一加筋黄土,劣化度排序为抗渗性>黏聚力>耐崩解性>内摩擦角。石灰与纤维的协同作用有效提升了黄土的长期稳定性,研究成果为西北地区黄土边坡坡面防护提供了试验支撑。

       

      Abstract: To investigate the deterioration rules of macroscopic properties of lime-fiber modified loess under wetting-drying cycles, the variations of shear strength, disintegration coefficient and permeability coefficient of the lime-fiber modified loess are analyzed through direct shear tests, disintegration tests and permeability tests. The results show that the cementitious substances generated by lime hydration can fill the pores inside fiber reinforcement soil, enhancing soil compaction while inhibiting the development of seepage channels. After 15 wetting-drying cycles, the disintegration coefficients of fiber-reinforced loess and lime–fiber reinforced loess increase by 6.5% and 10.7%, respectively, compared with those of untreated loess. Meanwhile, their permeability coefficients increase by 8.3% and 18.2%, respectively. The deterioration rate of macroscopic properties of lime-reinforced loess gradually slows down with the increase of wetting-drying cycles. The hyperbolic model can reflect the correlation relationship between the deterioration of macroscopic properties and the number of wetting-drying cycles. The macroscopic performance of lime-fiber-reinforced loess is significantly better than that of single reinforced loess, with the final deterioration degree ranking as follows: permeability resistance > cohesion > disintegration resistance > internal friction angle. The synergistic effect of lime and fiber effectively improves the long-term stability of loess and provides experimental support for the protection of loess slopes in Northwest China.

       

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