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    Zero-Inertial Recession for Kinematic-Wave Model

    Source: Journal of Irrigation and Drainage Engineering:;2011:;Volume ( 137 ):;issue: 004
    Author:
    Albert J. Clemmens
    ,
    Theodor Strelkoff
    DOI: 10.1061/(ASCE)IR.1943-4774.0000289
    Publisher: American Society of Civil Engineers
    Abstract: Kinematic-wave models of surface irrigation assume a fixed relationship between depth and discharge (typically, normal depth). When surface-irrigation inflow is cut off, the calculated upstream flow depth goes to zero, because the discharge is zero. For short time steps, use of the kinematic-wave model can create an incorrect water-surface profile. Issues include difficulty in solving the continuity equation in the first upstream cell and a calculated adverse water-surface profile. The kinematic-wave model produces a recession time at the upstream boundary that is too small, that can lead to incorrect calculation of recession times when water continues to recede from the surface. This problem becomes more severe for smaller values of bottom slope. In this paper, we present a zero-inertia approximation to the water-surface profile at cutoff, which can be extended to the start of recession, after which calculations continue with the kinematic-wave model.
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      Zero-Inertial Recession for Kinematic-Wave Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/65185
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    contributor authorAlbert J. Clemmens
    contributor authorTheodor Strelkoff
    date accessioned2017-05-08T21:52:52Z
    date available2017-05-08T21:52:52Z
    date copyrightApril 2011
    date issued2011
    identifier other%28asce%29ir%2E1943-4774%2E0000318.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/65185
    description abstractKinematic-wave models of surface irrigation assume a fixed relationship between depth and discharge (typically, normal depth). When surface-irrigation inflow is cut off, the calculated upstream flow depth goes to zero, because the discharge is zero. For short time steps, use of the kinematic-wave model can create an incorrect water-surface profile. Issues include difficulty in solving the continuity equation in the first upstream cell and a calculated adverse water-surface profile. The kinematic-wave model produces a recession time at the upstream boundary that is too small, that can lead to incorrect calculation of recession times when water continues to recede from the surface. This problem becomes more severe for smaller values of bottom slope. In this paper, we present a zero-inertia approximation to the water-surface profile at cutoff, which can be extended to the start of recession, after which calculations continue with the kinematic-wave model.
    publisherAmerican Society of Civil Engineers
    titleZero-Inertial Recession for Kinematic-Wave Model
    typeJournal Paper
    journal volume137
    journal issue4
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)IR.1943-4774.0000289
    treeJournal of Irrigation and Drainage Engineering:;2011:;Volume ( 137 ):;issue: 004
    contenttypeFulltext
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