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dc.contributor.authorA. C. Stamatopoulos
dc.contributor.authorP. C. Kotzias
dc.date.accessioned2017-05-08T20:38:06Z
dc.date.available2017-05-08T20:38:06Z
dc.date.copyrightMay 1996
dc.date.issued1996
dc.identifier.other%28asce%290733-9410%281996%29122%3A5%28408%29.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl/handle/yetl/21873
dc.description.abstractThis note describes slide failures of the inside slope of a water reservoir, following a prolonged period of heavy rainfall. The reservoir had just been completed and was empty. Sliding took place along the plane of the smooth-surfaced geomembrane high-density polyethylene (HDPE), which had been installed 0.4 m below the face of the slope to contain stored water. Sliding cannot be explained by gravity forces only. By considering the combined effect of gravity and seepage forces acting on the surface of the membrane at the time of sliding, under wet conditions, it was calculated that the coefficient of friction between the geomembrane and the nonplastic silty sand of the soil cover is between 0.325–0.360. Under wet conditions, either of these values agree with previously published coefficients of friction between HDPE geomembrane and sand, or between smooth-surfaced concrete and steel, and plastic silt.
dc.publisherAmerican Society of Civil Engineers
dc.titleEarth Slide on Geomembrane
dc.typeJournal Paper
dc.journal.volume122
dc.journal.issue5
dc.journal.titleJournal of Geotechnical Engineering
dc.identifier.doi10.1061/(ASCE)0733-9410(1996)122:5(408)
dc.treeJournal of Geotechnical Engineering:;1996:;Volume ( 122 ):;issue: 005
dc.contenttypeFulltext


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