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Pore water salinity effect on the intrinsic compression behaviour of artificial soft soils

机译:孔隙水盐度对人工软土固有压缩特性的影响

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摘要

The framework of the intrinsic compression behaviour of normally consolidated soft clay proposed by Burland (1990) is widely adopted in engineering practices. However, further investigations should be conducted on its validity in the coastal and offshore environments to verify the effect of pore water salinity. In the present work, oedometer tests were performed on remoulded artificial soft clays (mixtures of kaolin and bentonite with 0%, 5%, 10%, and 20% of bentonite by mass). The artificial clays were salinized with sodium chloride solutions at concentrations 0 mol/L (distilled water), 0.17 mol/L, 0.51 mol/L, 0.86 mol/L, and 1.70 mol/L at water contents equal to 1.0-1.5 times of the liquid limits. The results showed that the 'intrinsic' properties of clays, including the compression index C-c*(100-1000 kPa), void ratio e(100)*, and compression line based on the void index I-v, changed with the pore water salinity. Following the empirical correlation proposed by previous researchers, the decrease in C-c* caused by pore water salinity could be generally characterised by the liquid limit and void ratio at the liquid limit (e(L)). The dispersed correlation between the predicted e(100)* and the experimental results in this study were caused by the significant changes in e(0)/e(L), controlled by pore water salinity. The relationships between void index I-v and vertical stress sigma(v)' deviated from the intrinsic compression line (ICL) under the saline environment. For the artificial clay rich in smectite, the slopes of I-v-log sigma(v)' before yielding increased with pore water salinity at the initial water content. Pore water salinity affected the intrinsic compression behaviour of soft clays primarily composed of kaolinite to a lesser extent.
机译:Burland(1990)提出的通常固结的软粘土固有压缩特性的框架在工程实践中被广泛采用。但是,应进一步研究其在沿海和近海环境中的有效性,以验证孔隙水盐度的影响。在目前的工作中,对重塑的人造软粘土(高岭土和膨润土的质量百分比为0%,5%,10%和20%的膨润土的混合物)进行了里程表测试。在水含量等于水的1.0-1.5倍的情况下,用浓度为0 mol / L(蒸馏水),0.17 mol / L,0.51 mol / L,0.86 mol / L和1.70 mol / L的氯化钠溶液对人造粘土进行盐化。液体极限。结果表明,粘土的“固有”特性,包括压缩指数C-c *(100-1000 kPa),孔隙率e(100)*和基于孔隙指数I-v的压缩线,随孔隙水盐度的变化而变化。遵循先前研究人员提出的经验相关性,孔隙水盐度引起的C-c *下降通常可以通过液位极限和液位极限处的空隙率(e(L))来表征。预测e(100)*与本研究中实验结果之间的分散相关性是由孔隙水盐度控制的e(0)/ e(L)的显着变化引起的。在盐环境下,空隙指数I-v与垂直应力sigma(v)'之间的关系偏离了固有压缩线(ICL)。对于富含绿土的人造粘土,在初始含水量下,I-v-log sigma(v)'的斜率随孔隙水盐度的增加而增加。孔隙水的盐度在较小程度上影响了主要由高岭石组成的软粘土的固有压缩行为。

著录项

  • 来源
    《Applied clay science》 |2018年第12期|299-306|共8页
  • 作者单位

    Southeast Univ, Transportat Coll, Inst Geotech Engn, SEU Ave 2, Nanjing 211189, Jiangsu, Peoples R China;

    Southeast Univ, Transportat Coll, Inst Geotech Engn, SEU Ave 2, Nanjing 211189, Jiangsu, Peoples R China;

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

    Tongji Univ, Sch Civil Engn, Shanghai, Peoples R China;

    Southeast Univ, Transportat Coll, Inst Geotech Engn, SEU Ave 2, Nanjing 211189, Jiangsu, Peoples R China;

    Guangxi Univ, Coll Mech Engn, Nanning, Peoples R China;

  • 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

    Artificial soft clay; Pore water salinity effect; Intrinsic compression behaviour; Particle flocculation;

    机译:人造软黏土;孔隙水盐度效应;固有压缩行为;颗粒絮凝;

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