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    Gravity Current of Fluid Mud on Sloping Bed

    Source: Journal of Hydraulic Engineering:;1996:;Volume ( 122 ):;issue: 012
    Author:
    Thijs van Kessel
    ,
    C. Kranenburg
    DOI: 10.1061/(ASCE)0733-9429(1996)122:12(710)
    Publisher: American Society of Civil Engineers
    Abstract: The presence of fluid mud on inclined beds can cause high transport rates because of sliding due to the gravity force. In the present paper, gravity currents of fluid mud on sloping beds have been studied experimentally; velocity and concentration profiles were measured at two positions in a laboratory flume. The model fluid mud was prepared by suspending china clay in tap water; bulk densities varied from 1,050 to 1,230 kg/m
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      Gravity Current of Fluid Mud on Sloping Bed

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    contributor authorThijs van Kessel
    contributor authorC. Kranenburg
    date accessioned2017-05-08T20:42:29Z
    date available2017-05-08T20:42:29Z
    date copyrightDecember 1996
    date issued1996
    identifier other%28asce%290733-9429%281996%29122%3A12%28710%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/24236
    description abstractThe presence of fluid mud on inclined beds can cause high transport rates because of sliding due to the gravity force. In the present paper, gravity currents of fluid mud on sloping beds have been studied experimentally; velocity and concentration profiles were measured at two positions in a laboratory flume. The model fluid mud was prepared by suspending china clay in tap water; bulk densities varied from 1,050 to 1,230 kg/m
    publisherAmerican Society of Civil Engineers
    titleGravity Current of Fluid Mud on Sloping Bed
    typeJournal Paper
    journal volume122
    journal issue12
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1996)122:12(710)
    treeJournal of Hydraulic Engineering:;1996:;Volume ( 122 ):;issue: 012
    contenttypeFulltext
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