Abstract

Systems of sealing of containers or retention pounds are often associated to drainage layers for leachate recovery. The drainage layer can be installed either above the sealing layer or below it. In this paper, double layered columns of alluvia and clayey sand or of alluvia and clay are made up to run infiltration tests. A follow-up of the water content is implemented during the infiltration in multi-layer columns by using TDR probes. The values and changes in infiltration rate are different if the drainage layer is above or below the sealing layer. It is found that the drainage layer saturation is delayed when the sealing layer is above but the equilibrium water content remains the same for the both configuration. The electrical measurements in the drainage layers prove that the increase rate of the solute accumulation is the same for the both configuration and the same equilibrium solute concentration is reached. The measured coefficient of permeability of the double-layered becomes five times higher when the drainage layer is below the sealing layer. The position of the drainage layer influences the infiltration rate, the water and solute migration. The change in coefficient of permeability must be taken into account for the assessment of the flux of pollutant across a barrier system.

Highlights

  • The systems of sealing of containers or retention pounds are often associated with a drainage layer for leachate recovery

  • Columns made up either of a layer of alluvium and of clayey sand or of a layer of alluvium and of clay are prepared for the infiltration tests

  • The infiltration rate is used to observe the influence of the drainage layer above or below the sealing layer

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Summary

Introduction

The systems of sealing of containers or retention pounds are often associated with a drainage layer for leachate recovery. The purpose of the tests carried out in this study is to observe the influence that the presence of the drainage layer has on the evolution of the hydrodynamic parameters of the sealing layer during the saturation process. Columns made up either of a layer of alluvium and of clayey sand or of a layer of alluvium and of clay are prepared for the infiltration tests. The unsaturated soils are compacted in individual rings to ensure the homogeneity of the density of each layer of the doublelayered or the multi-layer one. The results of the tests allow the comparison of the curves of infiltration of full-layer and multi-layered of unsaturated soil, to describe the profile forms in the double-layered ones and to compare the coefficients of permeability. By using TDR measurement of electrical conductivity, pollutant migration and retention is described

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