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    Non‐steady‐Flow Type Curves for Strip Aquifers with Constant Drawdown

    Source: Journal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 004
    Author:
    Halil Onder
    DOI: 10.1061/(ASCE)0733-9437(1994)120:4(732)
    Publisher: American Society of Civil Engineers
    Abstract: A type‐curve method to determine aquifer parameters from a constant‐drawdown test at a drain in a finite strip aquifer is described. An available solution in the form of complementary error functions to one‐dimensional, non‐steady flow toward a drain, under constant drawdown condition in a strip aquifer bounded on the other side by an impervious formation, is used to define a drain function. Values of the drain function are calculated by using a polynomial approximation for the complementary error function and are tabulated, and a corresponding family of type curves is constructed for selected values of dimensionless distance along the width of the strip aquifer. The method is demonstrated through an application. The proposed match‐point procedure may be used to determine the aquifer parameters from observed drawdown values in an observation well in the strip aquifer and discharge data measured in the drain during constant drawdown canal pumping tests.
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      Non‐steady‐Flow Type Curves for Strip Aquifers with Constant Drawdown

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    http://yetl.yabesh.ir/yetl1/handle/yetl/27585
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    contributor authorHalil Onder
    date accessioned2017-05-08T20:48:01Z
    date available2017-05-08T20:48:01Z
    date copyrightJuly 1994
    date issued1994
    identifier other%28asce%290733-9437%281994%29120%3A4%28732%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/27585
    description abstractA type‐curve method to determine aquifer parameters from a constant‐drawdown test at a drain in a finite strip aquifer is described. An available solution in the form of complementary error functions to one‐dimensional, non‐steady flow toward a drain, under constant drawdown condition in a strip aquifer bounded on the other side by an impervious formation, is used to define a drain function. Values of the drain function are calculated by using a polynomial approximation for the complementary error function and are tabulated, and a corresponding family of type curves is constructed for selected values of dimensionless distance along the width of the strip aquifer. The method is demonstrated through an application. The proposed match‐point procedure may be used to determine the aquifer parameters from observed drawdown values in an observation well in the strip aquifer and discharge data measured in the drain during constant drawdown canal pumping tests.
    publisherAmerican Society of Civil Engineers
    titleNon‐steady‐Flow Type Curves for Strip Aquifers with Constant Drawdown
    typeJournal Paper
    journal volume120
    journal issue4
    journal titleJournal of Irrigation and Drainage Engineering
    identifier doi10.1061/(ASCE)0733-9437(1994)120:4(732)
    treeJournal of Irrigation and Drainage Engineering:;1994:;Volume ( 120 ):;issue: 004
    contenttypeFulltext
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