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    Earth Dam‐Canyon Interaction Effects for Obliquely Incident SH Waves

    Source: Journal of Geotechnical Engineering:;1993:;Volume ( 119 ):;issue: 011
    Author:
    Panos Dakoulas
    DOI: 10.1061/(ASCE)0733-9410(1993)119:11(1696)
    Publisher: American Society of Civil Engineers
    Abstract: Dam‐canyon interaction effects on the response of earth and rockfill dams built in narrow canyons are considered. An analytical closed‐form solution is used for a dam in a semicylindrical canyon, subjected to obliquely incident harmonic SH waves. The dam is idealized as linearly hysteretic elastic body deforming only in shear, while the canyon is modeled as an elastic half‐space. The model accounts in a rigorous way for the wave reflection and diffraction phenomena caused by the presence of the dam‐canyon system. It is shown that the motion amplification is considerably less for a dam in flexible canyon than for a dam in a rigid canyon and that the effects of radiation damping and asynchronous base motion may be very important. For oblique SH waves, the presence of antisymmetric terms in the solution may lead to response substantially higher than that induced by vertically propagating waves. Finally, as the canyon narrowness increases, the amplification at higher frequencies increases significantly for a rigid base, but it may decrease for a flexible base.
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      Earth Dam‐Canyon Interaction Effects for Obliquely Incident SH Waves

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    https://yetl.yabesh.ir/yetl1/handle/yetl/21172
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    contributor authorPanos Dakoulas
    date accessioned2017-05-08T20:36:45Z
    date available2017-05-08T20:36:45Z
    date copyrightNovember 1993
    date issued1993
    identifier other%28asce%290733-9410%281993%29119%3A11%281696%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/21172
    description abstractDam‐canyon interaction effects on the response of earth and rockfill dams built in narrow canyons are considered. An analytical closed‐form solution is used for a dam in a semicylindrical canyon, subjected to obliquely incident harmonic SH waves. The dam is idealized as linearly hysteretic elastic body deforming only in shear, while the canyon is modeled as an elastic half‐space. The model accounts in a rigorous way for the wave reflection and diffraction phenomena caused by the presence of the dam‐canyon system. It is shown that the motion amplification is considerably less for a dam in flexible canyon than for a dam in a rigid canyon and that the effects of radiation damping and asynchronous base motion may be very important. For oblique SH waves, the presence of antisymmetric terms in the solution may lead to response substantially higher than that induced by vertically propagating waves. Finally, as the canyon narrowness increases, the amplification at higher frequencies increases significantly for a rigid base, but it may decrease for a flexible base.
    publisherAmerican Society of Civil Engineers
    titleEarth Dam‐Canyon Interaction Effects for Obliquely Incident SH Waves
    typeJournal Paper
    journal volume119
    journal issue11
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1993)119:11(1696)
    treeJournal of Geotechnical Engineering:;1993:;Volume ( 119 ):;issue: 011
    contenttypeFulltext
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