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    Hydraulic Conductivity Tests on Compacted Clay

    Source: Journal of Geotechnical Engineering:;1985:;Volume ( 111 ):;issue: 004
    Author:
    Stephen S. Boynton
    ,
    David E. Daniel
    DOI: 10.1061/(ASCE)0733-9410(1985)111:4(465)
    Publisher: American Society of Civil Engineers
    Abstract: Permeability tests were performed in the laboratory on compacted clay to study the effects of type of permeameter, hydraulic anisotropy, diameter of test specimens, storage time, and desiccation cracking. Essentially identical hydraulic conductivities were measured with compaction‐mold, consolidation‐cell, and flexible‐wall permeameters. With good bonding between lifts, hydraulic conductivity was isotropic. Test specimens having a diameter of 15 cm were twice as permeable as specimens having a diameter of 4 cm, but this difference is too small to be of any consequence. There was no tendency for hydraulic conductivity to increase with increasing storage time. Desiccation cracks in compacted clay close only partially when the clay is moistened and permeated, unless substantial effective stresses are applied to aid in closing the cracks.
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      Hydraulic Conductivity Tests on Compacted Clay

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    https://yetl.yabesh.ir/yetl1/handle/yetl/19747
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    contributor authorStephen S. Boynton
    contributor authorDavid E. Daniel
    date accessioned2017-05-08T20:33:58Z
    date available2017-05-08T20:33:58Z
    date copyrightApril 1985
    date issued1985
    identifier other%28asce%290733-9410%281985%29111%3A4%28465%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/19747
    description abstractPermeability tests were performed in the laboratory on compacted clay to study the effects of type of permeameter, hydraulic anisotropy, diameter of test specimens, storage time, and desiccation cracking. Essentially identical hydraulic conductivities were measured with compaction‐mold, consolidation‐cell, and flexible‐wall permeameters. With good bonding between lifts, hydraulic conductivity was isotropic. Test specimens having a diameter of 15 cm were twice as permeable as specimens having a diameter of 4 cm, but this difference is too small to be of any consequence. There was no tendency for hydraulic conductivity to increase with increasing storage time. Desiccation cracks in compacted clay close only partially when the clay is moistened and permeated, unless substantial effective stresses are applied to aid in closing the cracks.
    publisherAmerican Society of Civil Engineers
    titleHydraulic Conductivity Tests on Compacted Clay
    typeJournal Paper
    journal volume111
    journal issue4
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1985)111:4(465)
    treeJournal of Geotechnical Engineering:;1985:;Volume ( 111 ):;issue: 004
    contenttypeFulltext
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