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    Green-Ampt One-Dimensional Infiltration from a Ponded Surface into a Heterogeneous Soil

    Source: Journal of Irrigation and Drainage Engineering:;2010:;Volume ( 136 ):;issue: 001
    Author:
    A. R. Kacimov
    ,
    S. Al-Ismaily
    ,
    A. Al-Maktoumi
    DOI: 10.1061/(ASCE)IR.1943-4774.0000121
    Publisher: American Society of Civil Engineers
    Abstract: Saturated hydraulic conductivity and wetting front pressure head (as soil properties) on an abrupt Green-Ampt front are assumed to increase and decrease with depth of a porous heterogeneous soil subject to a constant ponding or infiltration-evaporation depleted ponding on the surface. The corresponding Cauchy problem for a nonlinear ordinary differential equation describing the wetting front propagation in the soil profile is solved by computer algebra routines. Sensitivity of the cumulative infiltration to variation of hydraulic conductivity and capillarity is studied. A concave-convex infiltration graph is obtained for some values of parameters of the assumed exponential growth/decay of conductivity/capillarity. Texture of soil samples collected from a pedon is used for calculation of conductivity from a pedotransfer function. Synthesis of heterogeneity resulting in a specified front dynamics is discussed.
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      Green-Ampt One-Dimensional Infiltration from a Ponded Surface into a Heterogeneous Soil

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    https://yetl.yabesh.ir/yetl1/handle/yetl/65005
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    contributor authorA. R. Kacimov
    contributor authorS. Al-Ismaily
    contributor authorA. Al-Maktoumi
    date accessioned2017-05-08T21:52:37Z
    date available2017-05-08T21:52:37Z
    date copyrightJanuary 2010
    date issued2010
    identifier other%28asce%29ir%2E1943-4774%2E0000149.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/65005
    description abstractSaturated hydraulic conductivity and wetting front pressure head (as soil properties) on an abrupt Green-Ampt front are assumed to increase and decrease with depth of a porous heterogeneous soil subject to a constant ponding or infiltration-evaporation depleted ponding on the surface. The corresponding Cauchy problem for a nonlinear ordinary differential equation describing the wetting front propagation in the soil profile is solved by computer algebra routines. Sensitivity of the cumulative infiltration to variation of hydraulic conductivity and capillarity is studied. A concave-convex infiltration graph is obtained for some values of parameters of the assumed exponential growth/decay of conductivity/capillarity. Texture of soil samples collected from a pedon is used for calculation of conductivity from a pedotransfer function. Synthesis of heterogeneity resulting in a specified front dynamics is discussed.
    publisherAmerican Society of Civil Engineers
    titleGreen-Ampt One-Dimensional Infiltration from a Ponded Surface into a Heterogeneous Soil
    typeJournal Paper
    journal volume136
    journal issue1
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)IR.1943-4774.0000121
    treeJournal of Irrigation and Drainage Engineering:;2010:;Volume ( 136 ):;issue: 001
    contenttypeFulltext
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