压实
土壤水分
岩土工程
路基
饱和(图论)
含水量
环境科学
土壤压实
堆积密度
土壤科学
饱和度
强夯法
地质学
数学
组合数学
作者
Satoru Shimobe,Giovanni Spagnoli
标识
DOI:10.1144/qjegh2019-130
摘要
Soil compaction is an important operation during the construction of road embankments, railway subgrade, earth dams and compacted clay liners for waste disposal. Soil compaction is usually controlled based on the ratio of the dry density of the soil to the soil water content. However, this relationship presents problems in both the laboratory and in the field when using excess compaction energy levels in cohesive soils with a high natural water content, including differences in the compaction energy levels and a reduction in strength as a result of over-compaction. The compaction curve, which considered the compaction energy levels, is usually unknown in the field and the main factors influencing the stiffness and strength of compacted soils are the dry density and the degree of saturation. We show here compaction results for soils in terms of the dry density and degree of saturation and introduce the concept of an optimum compaction line.
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