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    Seismic Lateral Pressures in Soils with Cohesion

    Source: Journal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 007
    Author:
    R. Richards, Jr.
    ,
    X. Shi
    DOI: 10.1061/(ASCE)0733-9410(1994)120:7(1230)
    Publisher: American Society of Civil Engineers
    Abstract: A full‐range, elastic‐plastic solution for seismic stresses in the free field is obtained for an ideal Mohr‐Coulomb material with cohesion. In addition, the effect of uniform surface tractions are included as are both constant vertical and horizontal acceleration components. Moreover, the basic equations are general in that they include both the active and passive cases where the lateral boundaries deform in a similar fashion but move less or more in magnitude than the free field dictates. Thus, this solution can be used directly to determine the seismic lateral pressures on walls or, for the special case when no wall is needed, the critical seismic height of a vertical cut in a cohesive soil. Conversely, the equations can be used to find the critical acceleration level at which a wall with a given factor of safety will move in an earthquake. Finally, once this critical earthquake intensity level is determined, the actual incremental accumulation of displacement of a given wall can be calculated by the simple sliding‐block approach or a wall can be designed to limit the seismic displacement to an acceptable level.
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      Seismic Lateral Pressures in Soils with Cohesion

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/21468
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    • Journal of Geotechnical Engineering

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    contributor authorR. Richards, Jr.
    contributor authorX. Shi
    date accessioned2017-05-08T20:37:18Z
    date available2017-05-08T20:37:18Z
    date copyrightJuly 1994
    date issued1994
    identifier other%28asce%290733-9410%281994%29120%3A7%281230%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/21468
    description abstractA full‐range, elastic‐plastic solution for seismic stresses in the free field is obtained for an ideal Mohr‐Coulomb material with cohesion. In addition, the effect of uniform surface tractions are included as are both constant vertical and horizontal acceleration components. Moreover, the basic equations are general in that they include both the active and passive cases where the lateral boundaries deform in a similar fashion but move less or more in magnitude than the free field dictates. Thus, this solution can be used directly to determine the seismic lateral pressures on walls or, for the special case when no wall is needed, the critical seismic height of a vertical cut in a cohesive soil. Conversely, the equations can be used to find the critical acceleration level at which a wall with a given factor of safety will move in an earthquake. Finally, once this critical earthquake intensity level is determined, the actual incremental accumulation of displacement of a given wall can be calculated by the simple sliding‐block approach or a wall can be designed to limit the seismic displacement to an acceptable level.
    publisherAmerican Society of Civil Engineers
    titleSeismic Lateral Pressures in Soils with Cohesion
    typeJournal Paper
    journal volume120
    journal issue7
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1994)120:7(1230)
    treeJournal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 007
    contenttypeFulltext
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