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    Seepage from Canal to Asymmetric Drainages

    Source: Journal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 005
    Author:
    Abate T. Wolde‐Kirkos
    ,
    A. S. Chawla
    DOI: 10.1061/(ASCE)0733-9437(1994)120:5(949)
    Publisher: American Society of Civil Engineers
    Abstract: In practice, canals located on ridges seldom have symmetric drainages on either side. In this paper, exact solution of the problem of seepage from a canal in a homogeneous medium to asymmetric drains located at finite distance from the canal is presented. The problem is solved by the use of conformal mapping. Equations for seepage discharge and the shape of the free surface are given. The values of seepage discharge are given in the form of easy to use curves. The analysis indicates that the seepage losses increase with increase in bed width and decrease in distance and the lowering of the level of the drainages. If the level of the higher drainage is raised beyond a critical value, this drainage becomes ineffective and seepage to this drainage will be zero. Fee surface rises if drainage on the other side is located at a farther and/or at a higher level.
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      Seepage from Canal to Asymmetric Drainages

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    http://yetl.yabesh.ir/yetl1/handle/yetl/27605
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    contributor authorAbate T. Wolde‐Kirkos
    contributor authorA. S. Chawla
    date accessioned2017-05-08T20:48:03Z
    date available2017-05-08T20:48:03Z
    date copyrightSeptember 1994
    date issued1994
    identifier other%28asce%290733-9437%281994%29120%3A5%28949%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/27605
    description abstractIn practice, canals located on ridges seldom have symmetric drainages on either side. In this paper, exact solution of the problem of seepage from a canal in a homogeneous medium to asymmetric drains located at finite distance from the canal is presented. The problem is solved by the use of conformal mapping. Equations for seepage discharge and the shape of the free surface are given. The values of seepage discharge are given in the form of easy to use curves. The analysis indicates that the seepage losses increase with increase in bed width and decrease in distance and the lowering of the level of the drainages. If the level of the higher drainage is raised beyond a critical value, this drainage becomes ineffective and seepage to this drainage will be zero. Fee surface rises if drainage on the other side is located at a farther and/or at a higher level.
    publisherAmerican Society of Civil Engineers
    titleSeepage from Canal to Asymmetric Drainages
    typeJournal Paper
    journal volume120
    journal issue5
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)0733-9437(1994)120:5(949)
    treeJournal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 005
    contenttypeFulltext
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