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    Granular-Fluid Chute Flow: Experimental and Numerical Observations

    Source: Journal of Hydraulic Engineering:;1995:;Volume ( 121 ):;issue: 004
    Author:
    Juan A. Garcia Aragon
    DOI: 10.1061/(ASCE)0733-9429(1995)121:4(355)
    Publisher: American Society of Civil Engineers
    Abstract: Equations of motion and boundary conditions for a flowing granular-fluid mixture, both based in the kinetic theory for granular flow, are here extended to allow for drag forces resulting from the interstitial fluid that cushions interparticle collisions and particle-wall collisions. Frictional stresses produced when long-term contacts are present and fluid turbulent fluctuations are introduced in the model. The results are compared with measurements from an experimental chute in which the inclination, the solids flow rate, and the fluid flow rate are all varied. The results show that for the same physical conditions (slope, channel roughness, and particle size) there is a value of concentration at which the ratio of collisional stresses over total stresses is a maximum. The theory is found to give a good qualitative account of the observed behavior.
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      Granular-Fluid Chute Flow: Experimental and Numerical Observations

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    contributor authorJuan A. Garcia Aragon
    date accessioned2017-05-08T20:42:18Z
    date available2017-05-08T20:42:18Z
    date copyrightApril 1995
    date issued1995
    identifier other%28asce%290733-9429%281995%29121%3A4%28355%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/24123
    description abstractEquations of motion and boundary conditions for a flowing granular-fluid mixture, both based in the kinetic theory for granular flow, are here extended to allow for drag forces resulting from the interstitial fluid that cushions interparticle collisions and particle-wall collisions. Frictional stresses produced when long-term contacts are present and fluid turbulent fluctuations are introduced in the model. The results are compared with measurements from an experimental chute in which the inclination, the solids flow rate, and the fluid flow rate are all varied. The results show that for the same physical conditions (slope, channel roughness, and particle size) there is a value of concentration at which the ratio of collisional stresses over total stresses is a maximum. The theory is found to give a good qualitative account of the observed behavior.
    publisherAmerican Society of Civil Engineers
    titleGranular-Fluid Chute Flow: Experimental and Numerical Observations
    typeJournal Paper
    journal volume121
    journal issue4
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1995)121:4(355)
    treeJournal of Hydraulic Engineering:;1995:;Volume ( 121 ):;issue: 004
    contenttypeFulltext
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