In some applications of geosynthetic clay liners (GCLs), the bentonite layer component of the GCL is encapsulated between two geomembranes. One of the benefits of this configuration is to decrease the risk of shear strength decrease due to bentonite hydration. The liner thus formed is typically used to contain a liquid, such as water or leachate. If there is a defect in the upper geomembrane, some of the liquid initially contained above the upper geomembrane migrates into the bentonite. Similarly, if there is a defect in the lower geomembrane, some of the liquid initially contained in the soil underlying the lower geomembrane migrates into the bentonite. The liquid that has migrated into the bentonite then migrates laterally in the bentonite between the two geomembranes. The analyses presented in this paper provide analytical solutions for the one-dimensional and axisymmetrical cases. In each of the two cases, two types of analytical solution are provided: an equation that gives the time required for the hydration front to reach a certain distance from the geomembrane defect, and an equation that gives the rate of liquid migration through the defect. It appears that the time required for the hydration front to reach a relatively small distance (e.g. a few meters) is very long (i.e. of the order of decades). Therefore a very long time is required for the development of a large hydrated area that could significantly impact shear strength. Also, a very long time is required for liquid migrating through a defect in the upper geomembrane to reach a defect in the lower geomembrane, thereby creating a leakage path from the medium overlying the upper geomembrane to the medium underlying the lower geomembrane. The analyses also show that the rate of liquid migration through the upper geomembrane defect is very small compared with the rate of leakage through the same defect in the geomembrane component of a typical composite liner where the soil component is clay or a GCL. The results of these analyses demonstrate the effectiveness of a liner that consists of a layer of bentonite encapsulated between two geomembranes, and provide a method to quantify this effectiveness.
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August 2004
Research Article|
August 01 2004
Liquid migration in an encapsulated bentonite layer due to geomembrane defects
J. P. Giroud;
J. P. Giroud
Chairman Emeritus
1
GeoSyntec Consultants, JP GIROUD, INC.
5837 North Ocean Blvd, Ocean Ridge, FL 33435, USA
Telephone: +1 561 737 1642, Telefax: +1 561 733 2809
, E-mail: jpg@jpgiroud.com
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D. E. Daniel
D. E. Daniel
Professor and Dean
2
College of Engineering, University of Illinois
306 Engineering Hall, MC-266, 1308 West Green Street, Urbana, IL 61801, USA
Telephone: +1 217 333 2150, Telefax: +1 217 244 7705
, E-mail: dedaniel@uiuc.edu
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Publisher: Emerald Publishing
Received:
February 19 2004
Revision Received:
April 29 2004
Accepted:
May 02 2004
Online ISSN: 1751-7613
Print ISSN: 1072-6349
© 2004 Thomas Telford Ltd
2004
Geosynthetics International (2004) 11 (4): 311–329.
Article history
Received:
February 19 2004
Revision Received:
April 29 2004
Accepted:
May 02 2004
Citation
Giroud JP, Daniel DE (2004), "Liquid migration in an encapsulated bentonite layer due to geomembrane defects". Geosynthetics International, Vol. 11 No. 4 pp. 311–329, doi: https://doi.org/10.1680/gein.2004.11.4.311
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