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Characterizing drying-induced clayey soil desiccation cracking process using electrical resistivity method

机译:用电阻率法表征干燥引起的黏性土壤干燥开裂过程

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摘要

Desiccation cracking process negatively impacts both mechanical and hydraulic properties of clayey soils. Traditional methods applied for the characterization of soil cracking behaviors are mainly based on visual inspections or destructive approaches. The electrical resistivity method provides a non-destructive, sensitive and continuous evaluation of the spatiotemporal variations of many soil physical properties. In this study, an integrated experimental setup is configured to simultaneously capture the evolution of temperature, relative humidity, water content, crack morphology, and apparent electrical resistivity in clay during continuous drying. Apparent electrical resistivity measurements at 1.0 cm electrode spacing are carried out to detect the initiation, propagation and coalescence of desiccation cracks. Image processing quantitatively describes the geometrical characteristics of shrinkage surface crack patterns. Experimental results indicate the strong correlation between the measured apparent electrical resistivity and cracking behavior of soil. As water content decreases during drying, the apparent electrical resistivity of initially saturated clayey soil decreases first before the onset of desiccation cracking, and then transits into the increasing trend. The evolution of apparent electrical resistivity in clayey soil is dominated by two competing effects, with one originated from the volumetric shrinkage-induced closer packing of soil fabric and higher concentration of ions in pore fluids, and another from the evaporation induced water loss associated with hydration film contraction and desiccation crack insulation. The electrical resistivity method is an effective technique to characterize the development of desiccation cracks, and particularly reliable to map their positions. This study is expected to improve the fundamental understanding of desiccation cracking mechanisms in soils and provide insights on soil characterizations for enhanced stability and performance of earthwork structures.
机译:干燥开裂过程会对黏性土壤的机械和水力性质产生负面影响。用于表征土壤开裂行为的传统方法主要基于目视检查或破坏性方法。电阻率方法可对许多土壤物理特性的时空变化进行无损,灵敏和连续的评估。在这项研究中,配置了一个集成的实验装置,以同时捕获在连续干燥过程中温度,相对湿度,水分,裂缝形态和表观电阻率的变化。进行电极间距为1.0 cm的表观电阻率测量,以检测干燥裂纹的萌生,传播和聚结。图像处理定量地描述了收缩表面裂纹图案的几何特征。实验结果表明,测得的表观电阻率与土壤的开裂行为之间具有很强的相关性。随着干燥过程中水含量的降低,最初饱和的黏性土的表观电阻率在干燥裂纹开始之前先降低,然后转变为增加的趋势。黏性土壤中表观电阻率的变化主要受两种竞争效应的影响,一种是由于体积收缩引起的土壤织物紧密堆积和离子在孔隙流体中的浓度较高,另一种则是由于蒸发引起的与水化有关的失水薄膜的收缩和干燥裂纹的保温。电阻率法是表征干燥裂纹发展的有效技术,并且特别可靠地绘制了它们的位置。这项研究有望增进对土壤干燥裂纹机理的基本理解,并为增强土工结构的稳定性和性能提供有关土壤特性的见解。

著录项

  • 来源
    《Applied clay science》 |2018年第2期|101-112|共12页
  • 作者单位

    Nanjing Univ, Sch Earth Sci & Engn, 163 Xianlin Rd, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Earth Sci & Engn, 163 Xianlin Rd, Nanjing 210023, Jiangsu, Peoples R China;

    Rowan Univ, Dept Civil & Environm Engn, 201 Mullica Hill Rd, Glassboro, NJ 08028 USA;

    Nanjing Univ, Sch Earth Sci & Engn, 163 Xianlin Rd, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Earth Sci & Engn, 163 Xianlin Rd, Nanjing 210023, Jiangsu, Peoples R China;

    Nanjing Univ, Sch Earth Sci & Engn, 163 Xianlin Rd, Nanjing 210023, Jiangsu, 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

    Clayey soil; Electrical resistivity method; Desiccation cracking; Crack pattern characterization; Image processing technique; Evaporation;

    机译:黏土;电阻率法;干燥裂纹;裂缝特征;图像处理技术;蒸发;
  • 入库时间 2022-08-17 13:53:22

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