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    Dynamic Lateral Pressures Due to Saturated Backfills on Rigid Walls

    Source: Journal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 010
    Author:
    Isao Ishibashi
    ,
    Makoto Osada
    ,
    Tatsuo Uwabe
    DOI: 10.1061/(ASCE)0733-9410(1994)120:10(1747)
    Publisher: American Society of Civil Engineers
    Abstract: One‐directional (horizontal) shaking‐table experiments were conducted on one sandy and two cohesive saturated backfills to investigate the dynamic water and total lateral pressures against rigid nonyielding walls during earthquakes. It was found that the dynamic water pressure against the wall is generated due to two different sources. The first source is Westergaard‐type, which is due to the flow of free water in nondeformable backfill soil skeleton and the second is due to the deformability of backfill soil skeleton under undrained conditions. For highly permeable backfill soils, the first source dominates in the generation of pore pressure and the second source dominates for cohesive backfills. The magnitude of the first type of dynamic water pressure is expressed as a function of the parameter
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      Dynamic Lateral Pressures Due to Saturated Backfills on Rigid Walls

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/21334
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    • Journal of Geotechnical Engineering

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    contributor authorIsao Ishibashi
    contributor authorMakoto Osada
    contributor authorTatsuo Uwabe
    date accessioned2017-05-08T20:37:03Z
    date available2017-05-08T20:37:03Z
    date copyrightOctober 1994
    date issued1994
    identifier other%28asce%290733-9410%281994%29120%3A10%281747%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/21334
    description abstractOne‐directional (horizontal) shaking‐table experiments were conducted on one sandy and two cohesive saturated backfills to investigate the dynamic water and total lateral pressures against rigid nonyielding walls during earthquakes. It was found that the dynamic water pressure against the wall is generated due to two different sources. The first source is Westergaard‐type, which is due to the flow of free water in nondeformable backfill soil skeleton and the second is due to the deformability of backfill soil skeleton under undrained conditions. For highly permeable backfill soils, the first source dominates in the generation of pore pressure and the second source dominates for cohesive backfills. The magnitude of the first type of dynamic water pressure is expressed as a function of the parameter
    publisherAmerican Society of Civil Engineers
    titleDynamic Lateral Pressures Due to Saturated Backfills on Rigid Walls
    typeJournal Paper
    journal volume120
    journal issue10
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1994)120:10(1747)
    treeJournal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 010
    contenttypeFulltext
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