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EFFECTS OF Cu2+ CONCENTRATION AND CONFINING PRESSURE ON THE HYDRAULIC CONDUCTIVITY OF SATURATED CLAY SOILS

机译:Cu 2+浓度和围压对饱和粘土土壤水力传导率的影响

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摘要

Hydraulic conductivity is a principal standard used to judge whether a clay liner is able to prevent leakage of leachates. The purpose of this investigation was to study the changes in permeability caused by two factors. One factor that regulates permeability of clay is the reaction that occurs between clays and chemicals when saturated clay soils are subjected to the permeation of heavy metal cations such as Cu2+. The other factor influencing the permeability of clay is the confining pressure exerted on clay samples. Hydraulic conductivity experiments were performed using a flexible wall permeameter in order to determine the effects of confining pressure and Cu2+ concentration on the permeability of saturated clay soils. The experiments were performed by varying one of two conditions in two sets of experiments: (1) In the first set of experiments, the soil samples were subjected to different confining pressures while the permeant concentration was kept constnnt; and (2) In the second set of experiments, the permeant concentrations were varied while the soil samples were subjected to the same confining pressure. It was observed that when the CuCl2 concentration remained constant (5.0g/L), the hydraulic conductivity of clay soil to water/CuCl2 mixtures was slightly greater than that to pure water. Meanwhile, when the confining pressure increased, there was a corresponding decrease in the reduction of hydraulic conductivity. Changing the properties of the permeant fluid had little influence on the permeability of soil samples when the confining pressure was over 600kPa. Under conditions where the confining pressure was kept constant while the concentrations of permeant were varied, the results showed that the void ratio and the hydraulic conductivity of soil slightly decreased when the solution concentration increased and when the CuCl2 concentration was less than 0.5g/L. However, the opposite effect occurred once the CuCl2 concentration increased over 0.5g/L. The test results showed that as the permeant concentration increased, both the void ratio and hydraulic conductivity values increased. Finally, a novel fitting formula was derived in order to describe the relationship among hydraulic conductivity, confining pressure and solution concentration.
机译:导水率是用来判断粘土衬里是否能够防止渗滤液泄漏的主要标准。这项研究的目的是研究由两个因素引起的渗透率变化。调节粘土渗透性的一个因素是当饱和的粘土土壤经过重金属阳离子(例如Cu2 +)的渗透时,粘土与化学物质之间发生的反应。影响粘土渗透性的另一个因素是施加在粘土样品上的围压。为了确定围压和Cu 2+浓度对饱和黏土渗透性的影响,使用挠性壁渗透仪进行了水力传导性实验。通过在两组实验中改变两个条件之一进行实验:(1)在第一组实验中,对土壤样品施加不同的围压,同时保持渗透浓度恒定; (2)在第二组实验中,当土壤样品受到相同的围压时,渗透物浓度发生变化。观察到,当CuCl2浓度保持恒定(5.0g / L)时,粘土对水/ CuCl2混合物的水力传导率略大于对纯水的水力传导率。同时,当围压升高时,水力传导率的降低相应降低。当围压超过600kPa时,改变渗透流体的性质对土壤样品的渗透性影响很小。结果表明,在改变渗透液浓度的同时保持围压恒定的条件下,当溶液浓度增加和CuCl2浓度小于0.5g / L时,孔隙率和土壤水力传导率略有下降。但是,一旦CuCl2浓度增加到0.5g / L以上,就会产生相反的效果。测试结果表明,随着渗透物浓度的增加,空隙率和水力传导率值均增加。最后,推导了一种新的拟合公式,以描述水力传导率,围压和溶液浓度之间的关系。

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  • 来源
    《Fresenius Environmental Bulletin》 |2015年第3期|755-763|共9页
  • 作者单位

    Beijing Univ Technol, Minist Educ & Beijing, Key Lab Urban Secur & Disaster Engn, Beijing 100124, Peoples R China;

    Beijing Univ Technol, Minist Educ & Beijing, Key Lab Urban Secur & Disaster Engn, Beijing 100124, Peoples R China;

    Beijing Univ Technol, Minist Educ & Beijing, Key Lab Urban Secur & Disaster Engn, Beijing 100124, Peoples R China;

    Beijing Univ Technol, Minist Educ & Beijing, Key Lab Urban Secur & Disaster Engn, Beijing 100124, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    permeant concentration; confining pressure; heavy metal cations; hydraulic conductivity;

    机译:渗透浓度;围压;重金属阳离子;水电导率;

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