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    Hydraulic Conditions Required to Move Unanchored Residue Materials

    Source: Journal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 003
    Author:
    J. E. Gilley
    ,
    E. R. Kottwitz
    ,
    G. A. Wieman
    DOI: 10.1061/(ASCE)0733-9437(1994)120:3(591)
    Publisher: American Society of Civil Engineers
    Abstract: Hydraulic conditions required to initiate movement of unanchored residue materials are identified in the present study. Selected amounts of corn, cotton, pine needles, sorghum, soybean, sunflower, and wheat residue are placed in a flume on a sand surface, and flow is then introduced at the top of the flume in progressive increments. The discharge rate and flow velocity necessary to cause residue movement are determined. The ratio of critical flow depth to residue diameter, critical Reynolds number, critical shear stress, dimensionless shear stress, and boundary Reynolds number are calculated from hydraulic measurements. Regression equations are developed to relate dimensionless shear stress to boundary Reynolds number and residue diameter. Boundary Reynolds number, in turn, is related to residue diameter and cover. Close agreement is found between predicted and actual parameter values obtained from the regression relations. The regression equations can be used to estimate the beginning of motion for other residue materials if residue diameter and cover are known.
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      Hydraulic Conditions Required to Move Unanchored Residue Materials

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/27563
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    • Journal of Irrigation and Drainage Engineering

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    contributor authorJ. E. Gilley
    contributor authorE. R. Kottwitz
    contributor authorG. A. Wieman
    date accessioned2017-05-08T20:47:59Z
    date available2017-05-08T20:47:59Z
    date copyrightMay 1994
    date issued1994
    identifier other%28asce%290733-9437%281994%29120%3A3%28591%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/27563
    description abstractHydraulic conditions required to initiate movement of unanchored residue materials are identified in the present study. Selected amounts of corn, cotton, pine needles, sorghum, soybean, sunflower, and wheat residue are placed in a flume on a sand surface, and flow is then introduced at the top of the flume in progressive increments. The discharge rate and flow velocity necessary to cause residue movement are determined. The ratio of critical flow depth to residue diameter, critical Reynolds number, critical shear stress, dimensionless shear stress, and boundary Reynolds number are calculated from hydraulic measurements. Regression equations are developed to relate dimensionless shear stress to boundary Reynolds number and residue diameter. Boundary Reynolds number, in turn, is related to residue diameter and cover. Close agreement is found between predicted and actual parameter values obtained from the regression relations. The regression equations can be used to estimate the beginning of motion for other residue materials if residue diameter and cover are known.
    publisherAmerican Society of Civil Engineers
    titleHydraulic Conditions Required to Move Unanchored Residue Materials
    typeJournal Paper
    journal volume120
    journal issue3
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)0733-9437(1994)120:3(591)
    treeJournal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 003
    contenttypeFulltext
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