Lyell Collection

Quarterly Journal of Engineering Geology and Hydrogeology

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Philip, L.K.
Right arrow Articles by Ellard, H.T.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Quarterly Journal of Engineering Geology and Hydrogeology; 2002; v. 35; issue.4; p. 345-354;
DOI: 10.1144/1470-9236/2001-37
© 2002 Geological Society of London

Original Article

A field-based test cell examining clay desiccation in landfill liners

L.K. Philip1, H. Shimell2, P.J. Hewitt3 & H.T. Ellard4

1 1School of Earth Sciences, University of Leeds, Leeds, LS23 6AJ, UK
2 2Environmental Resources Management Ltd, 8 Cavendish Square, London W1G 0ER, UK
3 3GSE Lining Technology, 37 Regal Drive, Soham, Cambridgeshire, CB7 5BE, UK
4 4Viridor Waste Management, Great Western House, Station Approach, Taunton, TA1 1QW, UK

Desiccation of clays can lead to the development of cracks and this is an important issue for mineral barriers used in lining and capping of landfills. The mechanisms of post-compaction moisture loss in a clay layer are reviewed and the results from a field test cell investigating clay desiccation are presented. A large scale instrumented test cell was constructed comprising a clay layer overlain by a geomembrane. Parts of the test cell were covered with a stone protection layer and parts of the test cell were sloping. Temperatures throughout the clay layer, relative humidity just above the clay, ambient air temperatures and crack patterns and dimensions wereobserved during a 36 day summer period. The amount of cracking was quantified using various crack indices. Cracks in the covered and flat sections were minimal whereas in the sloping uncovered portion cracking was initiated rapidly and then spread until the network of cracks at the surface stabilized and further dryingresulted in crack depth propagation. The geomembrane, exposed to the sun, was found to have a significant heating effect on the soil below. Significant moisture was lost over the entire thickness of the exposed barrier resulting in a modelled flow through the barrier of 19 times the construction value. Immediate covering of the geomembrane was found to greatly reduce the temperature variations, moisture loss and cracking. The results are discussed in the context of current crack theories and implications for landfill design and construction.

Key Words: clay • earthworks • landfill • microcracks • soil mechanics




This article has been cited by other articles:


Home page
Environmental GeosciencesHome page
M. Nadeem and M. B. Dusseault
Geological engineering criteria for deep solids injection
Environmental Geosciences, 2007; 14: 61 - 77.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
F. C. Brassington
Developments in UK hydrogeology since 1974
Geological Society, London, Special Publications, 2004; 225: 363 - 385.
[Abstract] [PDF]