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Microstructural Interpretation of Water Content and Dry Density Influence on the DC-Electrical Resistivity of a Fine-Grained Soil

机译:水分和干密度的微观结构解释对细粒土壤直流电阻率的影响

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摘要

In geotechnical engineering, there is a need for an in situ technique for measuring density and water content of soils quickly, accurately and, preferably, in a non-destructive way. DC-electrical resistivity provides a method capable of addressing this need. A new resistivity-cell and a new experimental procedure were developed to assess the resistivity of compacted samples of a silty soil. The study was carried out over moisture content and compaction level ranges that are consistent with those acceptable in earthwork construction. In this laboratory work, the effects of dry density and gravimetric water content on the soil bulk resistivity are considered separately. Furthermore, the effect of air index on electrical resistivity is demonstrated. Our data exhibit two distinct trends separated by a "critical" water content which appears to fall very close to the standard Proctor optimum moisture content for this soil. This promising result cannot be generalized as it needs to be investigated on other soils. The experimental results are further analyzed within the context of a previously published soil microfabric model which distinguishes water phase, air phase, particles assumed to be "inert" and clayey aggregates. Two types of electrical conduction enable explaining the results: first, conduction occurring in the intra-aggregate voids, controlled by the charge density on the surface of clayey particles; and then, inter-aggregate conduction controlled by interstitial water resistivity. The relative effect of each type of conduction is shown to strongly depend on water content. Finally, an extrapolation at zero air void allows for presenting an interpretation of the intra-aggregate volume contribution to electrical conduction in dry states. This interpretation suggests a dilution effect on the adsorbed cation concentration within bound water, that is shown to be consistent with recently published research.
机译:在岩土工程中,需要一种原位技术来快速,准确地并且优选地以无损方式测量土壤的密度和含水量。直流电阻率提供了一种能够满足该需求的方法。开发了一种新的电阻率单元和新的实验程序来评估粉质土壤压实样品的电阻率。该研究是在与土方建筑可接受的湿度和压实度范围相一致的范围内进行的。在本实验室工作中,分别考虑了干密度和重量水含量对土壤体积电阻率的影响。此外,证明了空气指数对电阻率的影响。我们的数据显示出两个明显的趋势,这些趋势被“临界”含水量隔开,该含水量似乎非常接近该土壤的标准Proctor最佳含水量。这个有希望的结果不能一概而论,因为它需要在其他土壤上进行研究。在先前公布的土壤微结构模型的背景下进一步分析了实验结果,该模型区分了水相,空气相,假定为“惰性”的颗粒和黏土聚集体。两种类型的电导率可以解释结果:第一,发生在团聚体内部空隙中的电导率受粘质颗粒表面的电荷密度控制;然后,通过间隙水电阻率控制聚集体间的传导。每种类型的传导的相对作用都显示出强烈依赖于水含量。最后,在零气隙处的外推法可以解释干燥状态下聚集体内部体积对导电的贡献。这种解释表明对结合水中吸附的阳离子浓度有稀释作用,这与最近发表的研究一致。

著录项

  • 来源
    《Geotechnical testing journal》 |2011年第6期|p.694-707|共14页
  • 作者单位

    Departement Surveillance Eau et Ouvrage, Service Developpement, Materiel, Methode, Electricite de France (EDF), DTG, 21 Ave. de l'Europe, Fr-38000 Grenoble, France;

    rnPRES Universite Nantes Angers Le Mans, IFSTTAR, Departement Mesure, Auscultation et Calcul Scientifique, Route de Bouaye, 44340 Bouguenais, France;

    rnCharier S.A., Direction Recherche et Developpement Durable, 87-89, rue Louis Pasteur, Fr-44550 Montoir-de-Bretagne, France;

    rnDepartement Mesure, Auscultation et Calcul Scientifique, PRES Universite Nantes Angers Le Mans, IFSTTAR, Route de Bouaye, Fr-44340 Bouguenais, France;

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

    DC-electrical resistivity; gravimetric water content; dry density; compacted silty soil; clayey aggregates;

    机译:直流电阻率重量水分干密度压实粉土黏土骨料;
  • 入库时间 2022-08-18 00:12:02

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