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GROUND IMPROVEMENT OF INTERMEDIATE RECLAIMED LAND BY COMPACTION THROUGH CAVITY EXPANSION OF SAND PILES

机译:通过砂桩的空腔扩张压实来改善中间开垦土地

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References(26) Cited-By(5) The crushed Tertiary Period mudstone used as the geomaterial for the artificial reclaimed land in the Joetsu Region of Japan consists of coarse and fine fractions of about 50% each and is classified as an “intermediate soil.” Unlike sand or clay soils, no constitutive equations or sufficiently established design methods have been available until now for evaluating intermediate soils. This paper first utilizes the SYS Cam-clay model (Asaoka et al., 2002) to identify the soil profile of intermediate reclaimed land through comparison of laboratory test results with the calculated responses of the constitutive equation. Next, the soil profile obtained is used to carry out various soil-water coupled finite deformation analyses. The main conclusions reached are as follows: 1) The rates of decay/collapse of the soil structure, loss of overconsolidation, and evolution of anisotropy of the soil materials that constitute the Joetsu reclaimed land lie midway between those of typical sand and clay. 2) Ground improvement by cavity expansion of sand piles is effective in converting the reclaimed land from a highly structured ground having heavier overconsolidation to a lightly overconsolidated ground with a low degree of structure by increasing the confining pressures within the ground. In particular, the reduction in the specific volume of the soil elements in the vicinity of the sand piles becomes large. 3) In the case of small vertical displacement, the composite ground containing the sand piles exhibits a bearing capacity of about 1.5 times that of an unimproved ground, and in the case of large displacement, the bearing capacity is about 2 times larger.
机译:参考文献(26)引用(5)在日本上越地区用作人工开垦土地的土工材料的第三纪碎屑泥岩,由粗粒和细粒各占约50%组成,被归类为“中间土壤”。 ”与沙土或黏土不同,到目前为止,还没有本构方程或充分建立的设计方法可用于评估中间土壤。本文首先利用SYS Cam-clay模型(Asaoka et al。,2002),通过将实验室测试结果与本构方程的计算结果进行比较,来识别中耕地的土壤剖面。接下来,将获得的土壤剖面用于进行各种土壤-水耦合的有限变形分析。得出的主要结论如下:1)构成上越复垦土地的土壤结构的衰变/塌陷率,超固结损失和各向异性的演化都位于典型的沙土和粘土之间。 2)通过砂堆的空腔膨胀来改善地面可有效地通过增加地面内的围压将填海土地从过度固结的高度结构化地面转变为结构程度低的轻度过度固结的地面。特别地,在沙堆附近的土壤元素的比容的减小变得很大。 3)在垂直位移小的情况下,包含砂桩的复合地基的承载力约为未改良地面的1.5倍,在大位移的情况下,承载力约为2倍。

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