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首页> 外文期刊>Applied clay science >Sand fraction effect on hydro-mechanical behavior of sand-clay mixture
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Sand fraction effect on hydro-mechanical behavior of sand-clay mixture

机译:砂分数对砂土混合物水力学行为的影响

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摘要

The sand-clay mixture was prepared to simulate special soils with discontinuous gradations, e.g. the residual soils, clinosols or hydraulic filling soils. Incremental loading oedometer tests were conducted to investigate their hydro-mechanical behaviors. The results were first analyzed based on the plots in the semi-logarithmic planes (i.e. normalized void ratio by that at liquid limit versus vertical effective stress, and versus hydraulic conductivity). It appears that the normalized void ratio by that at liquid limit allows valuable and reliable normalization of the compressibility and permeability curves. To investigate the influence of sand fraction, a four phase model of sand-clay mixture was introduced, enabling the void ratios of clay and sand to be determined. Further analysis showed that the sand void ratio and the normalized clay void ratio by that at liquid limit are also suitable parameters to describe the sand skeleton formation. Moreover, the normalized clay void ratio by that at liquid limit is an appropriate parameter to describe the hydraulic behavior of soils with or without sand fraction. When the sand skeleton was partly formed, the vertical stress was partly supported by the skeleton resulting in a different compression behavior from that of common clays. The partial formation of skeleton was found to depend on the relative dimension of coarse to fine grains as well as the stress state. This implies that during compression the interaction between sand and clay evolves, from non-, partial- to complete sand skeleton, reaching at the end of the maximum void ratio of sand. (C) 2016 Elsevier B.V. All rights reserved.
机译:制备沙土混合物以模拟具有不连续渐变的特殊土壤,例如残留的土壤,斜质土或水硬性土壤。进行了增量载荷里程表测试,以研究其水力机械性能。首先基于半对数平面中的图分析结果(即通过在液体极限处的归一化空隙率与垂直有效应力以及对水力传导率的归一化空隙率)。似乎通过在液体极限处的归一化空隙率可以对压缩率和渗透率曲线进行有价值且可靠的归一化。为了研究砂分的影响,引入了砂土混合物的四相模型,可以确定粘土和砂的空隙率。进一步的分析表明,砂孔隙率和归一化粘土孔隙率(在液限处)也是描述砂骨架形成的合适参数。此外,通过在液体极限处的归一化粘土孔隙率是描述有或没有沙分数的土壤的水力行为的合适参数。当部分地形成砂骨架时,垂直应力部分地由骨架支撑,从而导致其压缩行为不同于普通粘土。发现骨架的部分形成取决于粗晶粒与细晶粒的相对尺寸以及应力状态。这意味着在压缩过程中,砂和粘土之间的相互作用会从非,部分到完整的砂骨架演化,并达到砂最大孔隙率的末端。 (C)2016 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Applied clay science》 |2017年第1期|355-361|共7页
  • 作者单位

    Southeast Univ, Sch Transportat, Inst Geotech Engn, Nanjing, Jiangsu, Peoples R China;

    Southeast Univ, Sch Transportat, Inst Geotech Engn, Nanjing, Jiangsu, Peoples R China;

    Ecole Ponts ParisTech, Lab Navier, CERMES, Marne La Vallee, France;

    Southeast Univ, Sch Transportat, Inst Geotech Engn, Nanjing, Jiangsu, Peoples R China;

    Univ Newcastle, ARC Ctr Excellence Geotech Sci & Engn, Callaghan, NSW, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sand-day mixture; Sand fraction; Hydro-mechanical behavior; Four-phase model; Sand skeleton formation;

    机译:沙天混合物;砂分;水力学行为;四相模型;砂骨架形成;成因;

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