粗粒含量对压实试验的影响

Badee Alshameri
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摘要

压实是使松散土壤变致密的一种机制。通过优化最佳含水率(OMC)和最大干密度(MDD),可以实现土壤的最大密实化。最大干密度和最佳含水率受几个参数的影响。粗含量(CC)是这些参数之一。本文研究了粗粒含量对压实参数(MDD、OMC)的影响。几种砂-高岭土混合物的粗含量从30%到80%不等,水分含量从12%到20%不等,用于检测CC、比重(Gs)、MDD、OMC和容重之间的关系。结果表明,CC、Gs、MDD、OMC与容重之间存在5种经验相关,且决定系数R2≥0.98。本研究与前人的比较表明,土壤类型和含水量对最大干密度、比重和粗含量经验相关方程的有效性有显著影响。结果表明,粗粒含量与最大干密度呈线性关系,MDD和Gs随CC的增加而增加,而最佳含水量与粗粒含量呈非线性关系,OMC随CC的增加而减小。
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Effect of Coarse Content on Compaction Test
The compaction is a mechanism to densify the loose soils. The maximum soil densification can be achieved by optimization of the desirable optimum moisture content (OMC) and maximum dry density (MDD). The maximum dry density and the optimum moisture content were affected by several parameters. The coarse content (CC) is one of these parameters. This paper studied the effect of the coarse content on the compaction parameters (MDD, OMC). Several sand-kaolin mixtures had coarse content ranged from 30 % to 80 % and moisture content ranged from 12% to 20% were used to inspect the relationship between CC, specific gravity (Gs), MDD, OMC, and bulk density. The results presented five empirical correlations with coefficient of determination (R2 ≥ 0.98) between CC, Gs, MDD, OMC and bulk density. The comparison between the current study and previous researchers indicated that both soil type and moisture content have significant effect on the efficiency of the empirical correlation equations between the maximum dry density, specific gravity, and coarse content. The results indicated a linear relationship between coarse content toward maximum dry density and specific gravity where both MDD and Gs increased with an increase CC. In contrary, the results showed non-linear relationship between optimum moisture content and coarse content where OMC decrease with an increase CC.
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