固结仪试验
破损
钙质的
岩土工程
压缩性
粘土矿物
地质学
含水量
粒子(生态学)
临界状态土力学
阿太堡极限
矿物学
材料科学
土壤科学
土壤水分
复合材料
工程类
海洋学
有限元法
结构工程
航空航天工程
古生物学
本构方程
作者
Dongsheng Xu,Huang Ming,Yang Zhou
标识
DOI:10.1061/(asce)gm.1943-5622.0001763
摘要
More and more oceanic projects involve calcareous sand–marine clay mixtures which behave totally different from pure calcareous sand and marine clay. The effect of clay content on the compression behavior of the calcareous sand–marine clay mixture is investigated in this study. The results reveal that the coefficient of volumetric compressibility mv will be affected significantly by the clay content at low stress state (i.e., vertical stress less than 600 kPa), but the influence of the clay content on mv can be neglected at high stress states. Further laboratory tests found that the effect of clay content on the creep behavior is negligible for a marine clay fraction of 30% or less, but the effect increases with clay contents larger than 30%. In addition, the particle breakage characteristics are investigated from particle size distributions before and after application of loading in oedometer tests. A general correlation is obtained from the test data to evaluate particle breakage ratio Br by clay content r and magnitude of load p. Finally, a modified conceptual model based on Lade’s transitional fine content (TFC) model is proposed to predict the transitional state of the mixture by considering volume change induced by the sand breakage. The model is used to analyze the critical clay content at transitional state based on some reasonable assumptions and a very good prediction can be obtained.
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