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On the Use of Skempton's Compression Index Equation

机译:关于Skempton压缩指数方程的使用

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In this study, an alternate approach to establish the e-log p relationships for clayey soils within a vertical pressure range of 10-1,000 kPa is discussed. Skempton's compression index equation correlating the liquid limit, w_L, and the compression index, C_c, and the reported equation correlating the void ratio at liquid limit, e_L, and the void ratio at a vertical pressure of 100 kPa, e_(100), by Burland (1990), were used to establish the e-log p relationships for several reconstituted normally consolidated clayey soils. Consolidation test results of 13 clayey soils covering a sufficiently wide range of liquid limit were selected from the literature. Also, consolidation tests were carried out on two highly expansive soils in this study. A comparison of the experimental consolidation test results with the calculated e-log p relationships in the current study indicated that in general, the agreements between the calculated relationships and the experimental results are good. The agreements were found to be slightly better for soils with liquid limits less than about 70%. A comparison of the calculated e-log p relationships in the current study with that determined following methods suggested by Nagaraj and Srinivasa Murthy (1983) and Burland (1990) showed that all the three methods yielded very similar results for soils with liquid limit less than 70%. For soils with liquid limits greater than 70%, the difference between the e-log p relationships calculated in this study and that following Burland (1990)'s method was insignificant, whereas Nagaraj and Srinivasa Murthy (1983)'s method slightly over-predicted the void ratios at larger vertical stresses.
机译:在这项研究中,讨论了在10-1,000 kPa的垂直压力范围内为黏性土壤建立e-log p关系的替代方法。 Skempton的压缩指数方程式将液体极限w_L与压缩指数C_c相关联,报告的方程式将液体极限下的空隙率e_L与垂直压力为100 kPa时的空隙率e_(100)关联起来Burland(1990),用于建立几种重构的通常固结的黏土的e-log p关系。从文献中选择了覆盖足够液体极限范围的13种黏土的固结测试结果。此外,在这项研究中,在两种高度膨胀的土壤上进行了固结测试。将当前实验中的固结测试结果与计算的e-log p关系进行比较表明,总体而言,计算的关系与实验结果之间的一致性很好。发现该协议对于液体含量低于约70%的土壤略胜一筹。将当前研究中计算的e-log p关系与根据Nagaraj和Srinivasa Murthy(1983)和Burland(1990)建议的方法确定的关系进行比较,结果表明,对于液体限度小于10%的土壤,这三种方法均产生非常相似的结果。 70%。对于液体极限值大于70%的土壤,本研究计算的e-log p关系与遵循Burland(1990)的方法之间的关系微不足道,而Nagaraj和Srinivasa Murthy(1983)的方法则略有不同。预测了较大垂直应力下的空隙率。

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