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    Dynamic Replacement and Mixing of Organic Soils with Sand Charges

    Source: Journal of Geotechnical Engineering:;1990:;Volume ( 116 ):;issue: 010
    Author:
    Kwang Wei Lo
    ,
    Peng Lee Ooi
    ,
    Seng‐Lip Lee
    DOI: 10.1061/(ASCE)0733-9410(1990)116:10(1463)
    Publisher: American Society of Civil Engineers
    Abstract: Field trials were initiated to investigate the feasibility of minimizing secondary as well as enforcing primary compression of peaty clays by dynamic replacement and mixing (DRM) with sand charges using conventional heavy tamping plant. Laboratory model tests were also conducted to amplify the field findings. The investigations have shown that DRM can transform in situ peaty clay deposits into an upper sand raft with pockets of peaty sand underlain by a fairly uniform layer of mixed sand and peat, where both sublayers have relatively insignificant secondary compression characteristics. Furthermore, for practical purposes, unique relationships may be established between degree of improvement of peaty clay after treatment (in terms of primary and secondary compression properties) and sand‐charge‐to‐compressible‐soil ratio
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      Dynamic Replacement and Mixing of Organic Soils with Sand Charges

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    http://yetl.yabesh.ir/yetl1/handle/yetl/20544
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    contributor authorKwang Wei Lo
    contributor authorPeng Lee Ooi
    contributor authorSeng‐Lip Lee
    date accessioned2017-05-08T20:35:31Z
    date available2017-05-08T20:35:31Z
    date copyrightOctober 1990
    date issued1990
    identifier other%28asce%290733-9410%281990%29116%3A10%281463%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/20544
    description abstractField trials were initiated to investigate the feasibility of minimizing secondary as well as enforcing primary compression of peaty clays by dynamic replacement and mixing (DRM) with sand charges using conventional heavy tamping plant. Laboratory model tests were also conducted to amplify the field findings. The investigations have shown that DRM can transform in situ peaty clay deposits into an upper sand raft with pockets of peaty sand underlain by a fairly uniform layer of mixed sand and peat, where both sublayers have relatively insignificant secondary compression characteristics. Furthermore, for practical purposes, unique relationships may be established between degree of improvement of peaty clay after treatment (in terms of primary and secondary compression properties) and sand‐charge‐to‐compressible‐soil ratio
    publisherAmerican Society of Civil Engineers
    titleDynamic Replacement and Mixing of Organic Soils with Sand Charges
    typeJournal Paper
    journal volume116
    journal issue10
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1990)116:10(1463)
    treeJournal of Geotechnical Engineering:;1990:;Volume ( 116 ):;issue: 010
    contenttypeFulltext
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