挤密桩桩间黄土挤密系数及其湿陷性分析
Investigation of the Compactness Coefficient and Collapsibility of Loess Between Compacted Piles
为研究挤密桩桩间黄土的湿陷性,考虑了挤密系数、饱和度对黄土湿陷性的影响,试验设置了挤密系数分别为 0.84、0.87、0.90、0.93,饱和度分别为 40%、50%、60%、70%,采用室内压缩试验测定了黄土湿陷系数、湿陷起始压力等指标,分析不同挤密系数和饱和度对黄土湿陷性的影响。结果表明,黄土挤密系数和饱和度对湿陷性的影响显著。随着挤密系数的增大,黄土湿陷系数呈减小趋势,湿陷起始压力呈增大趋势;随着饱和度的增大,黄土湿陷系数呈减小趋势,湿陷起始压力呈增大趋势。当黄土挤密系数增大到 0.93、饱和度大于 40% 时,黄土几乎不表现湿陷性,判定消除湿陷性的临界挤密系数为 0.93。
This study investigates the collapsibility of loess situated between compacted piles, focusing on the effects of the compactness coefficient and saturation levels on the loess’s behavior. The compactness coefficients were set at 0.84, 0.87, 0.90 and 0.93, respectively, while the saturation levels were established at 40%, 50%, 60% and 70%. Using indoor compression tests, it measured the collapsibility coefficient and the initial collapse pressure of the loess. The analysis reveals that both the compactness coefficient and saturation significantly influence the collapsibility of loess. As the compactness coefficient increases, the collapsibility coefficient decreases, whereas the initial collapse pressure increases. Similarly, an increase in saturation leads to a decrease in the collapsibility coefficient and an increase in the initial collapse pressure. Notably, when the compactness coefficient reaches 0.93 and the saturation exceeds 40%, the loess exhibits negligible collapsibility. Therefore, the critical compactness coefficient for eliminating collapsibility is determined to be 0.93. These findings provide a valuable reference for employing compacted piles to mitigate the collapsibility of loess.
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国家青年科学基金(51808302)
宁夏高等学校科学研究项目(NGY2018027)
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