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    Computer Modeling of Large Rock Slides

    Source: Journal of Geotechnical Engineering:;1986:;Volume ( 112 ):;issue: 003
    Author:
    F. J. Trunk
    ,
    J. D. Dent
    ,
    T. E. Lang
    DOI: 10.1061/(ASCE)0733-9410(1986)112:3(348)
    Publisher: American Society of Civil Engineers
    Abstract: A computer‐based analysis of the runout dynamics of the Madison Canyon rockslide of August 17, 1959, is reported. Three levels of computer representation of the flow are considered. First is a representation of the actual canyon profile, where the model assumes incompressible linear viscous flow. Second is a horizontal profile in which gravitational forces are input by components, and again the flow is approximated by a single viscosity model. Third is a horizontal profile, for which a two viscosity model approaching a Bingham material representation is used. Results of each model are compared to actual slide runout, debris distribution, and maximum speed of the flow. The biviscous model, which depicts an active basal flow layer, also has physical characteristics consistent with measurements made of the Madison Canyon slide following the event.
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      Computer Modeling of Large Rock Slides

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/19886
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    • Journal of Geotechnical Engineering

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    contributor authorF. J. Trunk
    contributor authorJ. D. Dent
    contributor authorT. E. Lang
    date accessioned2017-05-08T20:34:15Z
    date available2017-05-08T20:34:15Z
    date copyrightMarch 1986
    date issued1986
    identifier other%28asce%290733-9410%281986%29112%3A3%28348%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/19886
    description abstractA computer‐based analysis of the runout dynamics of the Madison Canyon rockslide of August 17, 1959, is reported. Three levels of computer representation of the flow are considered. First is a representation of the actual canyon profile, where the model assumes incompressible linear viscous flow. Second is a horizontal profile in which gravitational forces are input by components, and again the flow is approximated by a single viscosity model. Third is a horizontal profile, for which a two viscosity model approaching a Bingham material representation is used. Results of each model are compared to actual slide runout, debris distribution, and maximum speed of the flow. The biviscous model, which depicts an active basal flow layer, also has physical characteristics consistent with measurements made of the Madison Canyon slide following the event.
    publisherAmerican Society of Civil Engineers
    titleComputer Modeling of Large Rock Slides
    typeJournal Paper
    journal volume112
    journal issue3
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1986)112:3(348)
    treeJournal of Geotechnical Engineering:;1986:;Volume ( 112 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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