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    Flow Field Around Cones in Steady Penetration

    Source: Journal of Geotechnical Engineering:;1985:;Volume ( 111 ):;issue: 002
    Author:
    Mehmet T. Tumay
    ,
    Yalcin B. Acar
    ,
    Murat H. Cekirge
    ,
    Narayanan Ramesh
    DOI: 10.1061/(ASCE)0733-9410(1985)111:2(193)
    Publisher: American Society of Civil Engineers
    Abstract: An analytical solution is presented for the flow field around cones penetrating an inviscid and incompressible fluid. The stream function, velocity field, and strain rates around 18° and 60° cones advancing at a rate of 2 cm/sec are fully determined and presented. It is assumed that this strain rate field will give the first approximation to the in situ strains during penetration of very soft cohesive soils.
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      Flow Field Around Cones in Steady Penetration

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    https://yetl.yabesh.ir/yetl1/handle/yetl/72039
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    contributor authorMehmet T. Tumay
    contributor authorYalcin B. Acar
    contributor authorMurat H. Cekirge
    contributor authorNarayanan Ramesh
    date accessioned2017-05-08T22:08:07Z
    date available2017-05-08T22:08:07Z
    date copyrightFebruary 1985
    date issued1985
    identifier other31578462.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/72039
    description abstractAn analytical solution is presented for the flow field around cones penetrating an inviscid and incompressible fluid. The stream function, velocity field, and strain rates around 18° and 60° cones advancing at a rate of 2 cm/sec are fully determined and presented. It is assumed that this strain rate field will give the first approximation to the in situ strains during penetration of very soft cohesive soils.
    publisherAmerican Society of Civil Engineers
    titleFlow Field Around Cones in Steady Penetration
    typeJournal Paper
    journal volume111
    journal issue2
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1985)111:2(193)
    treeJournal of Geotechnical Engineering:;1985:;Volume ( 111 ):;issue: 002
    contenttypeFulltext
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