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    Nonuniform and Unsteady Solute Transport in Furrow Irrigation. I: Model Development

    Source: Journal of Irrigation and Drainage Engineering:;2010:;Volume ( 136 ):;issue: 006
    Author:
    Hugo Perea
    ,
    Theodor S. Strelkoff
    ,
    Floyd J. Adamsen
    ,
    Douglas J. Hunsaker
    ,
    Albert J. Clemmens
    DOI: 10.1061/(ASCE)IR.1943-4774.0000106
    Publisher: American Society of Civil Engineers
    Abstract: A cross-section-averaged advection-dispersion equation (ADE) model was developed to simulate the transport of fertilizer in furrow irrigation. The advection and dispersion processes were solved separately at each time step by implementing a method of characteristics with cubic-spline interpolation and a time-weighted finite-difference scheme, respectively. The upstream boundary condition was a prescribed concentration. Downstream, a zero-flux boundary condition during advance and a concentration gradient following completion of advance were prescribed. Local pseudosteady state was assumed in order to apply Fischer’s longitudinal dispersion equation under nonuniform and unsteady furrow flow conditions. Statistical parameters were used to evaluate the ADE model performance.
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      Nonuniform and Unsteady Solute Transport in Furrow Irrigation. I: Model Development

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    http://yetl.yabesh.ir/yetl1/handle/yetl/64989
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    contributor authorHugo Perea
    contributor authorTheodor S. Strelkoff
    contributor authorFloyd J. Adamsen
    contributor authorDouglas J. Hunsaker
    contributor authorAlbert J. Clemmens
    date accessioned2017-05-08T21:52:33Z
    date available2017-05-08T21:52:33Z
    date copyrightJune 2010
    date issued2010
    identifier other%28asce%29ir%2E1943-4774%2E0000133.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/64989
    description abstractA cross-section-averaged advection-dispersion equation (ADE) model was developed to simulate the transport of fertilizer in furrow irrigation. The advection and dispersion processes were solved separately at each time step by implementing a method of characteristics with cubic-spline interpolation and a time-weighted finite-difference scheme, respectively. The upstream boundary condition was a prescribed concentration. Downstream, a zero-flux boundary condition during advance and a concentration gradient following completion of advance were prescribed. Local pseudosteady state was assumed in order to apply Fischer’s longitudinal dispersion equation under nonuniform and unsteady furrow flow conditions. Statistical parameters were used to evaluate the ADE model performance.
    publisherAmerican Society of Civil Engineers
    titleNonuniform and Unsteady Solute Transport in Furrow Irrigation. I: Model Development
    typeJournal Paper
    journal volume136
    journal issue6
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)IR.1943-4774.0000106
    treeJournal of Irrigation and Drainage Engineering:;2010:;Volume ( 136 ):;issue: 006
    contenttypeFulltext
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