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    Drawdowns for Nonleaky Aquifer Flow with Storage in Finite‐Width Sink

    Source: Journal of Irrigation and Drainage Engineering:;1992:;Volume ( 118 ):;issue: 004
    Author:
    Louis H. Motz
    DOI: 10.1061/(ASCE)0733-9437(1992)118:4(645)
    Publisher: American Society of Civil Engineers
    Abstract: One-dimensional horizontal flow in a semi-infinite confined aquifer can be described in terms of mathematical solutions that relate the drawdown to aquifer parameters and the aquifer flow rate. A new analytical solution, that considers the effects of storage in a finite-width sink into which flow occurs from the aquifer, was developed for the nonleaky aquifer case. The solution is written in the form of exponential and complementary error functions, and a drain function is defined based on the solution. A type curve for the drain function is plotted, and aquifer parameters can be determined by matching drawdown data from observation wells to the type curve. Applications of this drain function and type-curve matching procedure would include analyzing aquifer drawdowns resulting from a canal pumping test, in which a significant part of the discharge from the canal was derived from water stored in the canal as well as from discharge from a nonleaky aquifer into the canal.
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      Drawdowns for Nonleaky Aquifer Flow with Storage in Finite‐Width Sink

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    http://yetl.yabesh.ir/yetl1/handle/yetl/27359
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    contributor authorLouis H. Motz
    date accessioned2017-05-08T20:47:38Z
    date available2017-05-08T20:47:38Z
    date copyrightJuly 1992
    date issued1992
    identifier other%28asce%290733-9437%281992%29118%3A4%28645%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/27359
    description abstractOne-dimensional horizontal flow in a semi-infinite confined aquifer can be described in terms of mathematical solutions that relate the drawdown to aquifer parameters and the aquifer flow rate. A new analytical solution, that considers the effects of storage in a finite-width sink into which flow occurs from the aquifer, was developed for the nonleaky aquifer case. The solution is written in the form of exponential and complementary error functions, and a drain function is defined based on the solution. A type curve for the drain function is plotted, and aquifer parameters can be determined by matching drawdown data from observation wells to the type curve. Applications of this drain function and type-curve matching procedure would include analyzing aquifer drawdowns resulting from a canal pumping test, in which a significant part of the discharge from the canal was derived from water stored in the canal as well as from discharge from a nonleaky aquifer into the canal.
    publisherAmerican Society of Civil Engineers
    titleDrawdowns for Nonleaky Aquifer Flow with Storage in Finite‐Width Sink
    typeJournal Paper
    journal volume118
    journal issue4
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)0733-9437(1992)118:4(645)
    treeJournal of Irrigation and Drainage Engineering:;1992:;Volume ( 118 ):;issue: 004
    contenttypeFulltext
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