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    Type Curves for Unsteady Flow to a Large-Diameter Well in Patchy Aquifers

    Source: Journal of Hydrologic Engineering:;2005:;Volume ( 010 ):;issue: 003
    Author:
    Mesut Çimen
    DOI: 10.1061/(ASCE)1084-0699(2005)10:3(200)
    Publisher: American Society of Civil Engineers
    Abstract: This paper analytically considers unsteady flow to a large-diameter well with the well storage in patchy aquifers that is cylindrically composed of two distinctive regions around the well with different hydraulic properties. The solution involves the usage of the independent variable transform. This approach gives, for both regions, the type curves that are dependent on the distance from the pumping well to the interface between two regions and the hydraulic parameter. The parameter is implied as the ratio of the transmissivity and the storage coefficients of two regions. A new well function expression—different from the well-known Theis well function—is defined to evaluate the field data. The function is seen as an approximation and is easily applicable to estimate the transmissivity and the storage coefficients of the patchy aquifers.
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      Type Curves for Unsteady Flow to a Large-Diameter Well in Patchy Aquifers

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    contributor authorMesut Çimen
    date accessioned2017-05-08T21:23:52Z
    date available2017-05-08T21:23:52Z
    date copyrightMay 2005
    date issued2005
    identifier other%28asce%291084-0699%282005%2910%3A3%28200%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/49856
    description abstractThis paper analytically considers unsteady flow to a large-diameter well with the well storage in patchy aquifers that is cylindrically composed of two distinctive regions around the well with different hydraulic properties. The solution involves the usage of the independent variable transform. This approach gives, for both regions, the type curves that are dependent on the distance from the pumping well to the interface between two regions and the hydraulic parameter. The parameter is implied as the ratio of the transmissivity and the storage coefficients of two regions. A new well function expression—different from the well-known Theis well function—is defined to evaluate the field data. The function is seen as an approximation and is easily applicable to estimate the transmissivity and the storage coefficients of the patchy aquifers.
    publisherAmerican Society of Civil Engineers
    titleType Curves for Unsteady Flow to a Large-Diameter Well in Patchy Aquifers
    typeJournal Paper
    journal volume10
    journal issue3
    journal titleJournal of Hydrologic Engineering
    identifier doi10.1061/(ASCE)1084-0699(2005)10:3(200)
    treeJournal of Hydrologic Engineering:;2005:;Volume ( 010 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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