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Leaky Aquifer Models to Simulate the Well Flow in Fractured Aquifers with Linear Interporosity Flow

机译:渗漏含水层模型以线性孔隙间流动模拟裂隙含水层的井流

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摘要

Following Hemker and Maas (1987) the models of two or three leaky aquifers are applied to simulate the flow to vertical wells operating in the fractured or dual porosity aquifers. The software WellTest (WT) (Szekely 2015) is used for calculating the drawdown and discharge rate variation. The comparative analysis with the independent analytical solutions by Boulton and Streltsova-Adams (1978), Warren and Root (1963), Kazemi et al. (1969) concluded with acceptable agreement between the WT simulation and the alternate calculation methods. The selected field tests have been conducted in fractured limestone aquifers. The pumping test west of Copenhagen shows an example of fractured aquifer with considerable negative skin effect at the well face. The flowing well Wafra W1 in Kuwait operates in the two-zone aquifer exhibiting sufficient vertical recharge via leakage beyond a circular domain of estimated radius of 2460 m.
机译:根据Hemker和Maas(1987)的模型,使用两个或三个漏水含水层的模型来模拟在裂隙或双重孔隙度含水层中运行的垂直井的流动。 WellTest(WT)软件(Szekely,2015年)用于计算压降和排放速率变化。 Boulton和Streltsova-Adams(1978),Warren和Root(1963),Kazemi等人使用独立的分析解决方案进行比较分析。 (1969年)得出结论,在WT模拟和替代计算方法之间可以接受。选定的现场测试已在裂缝性石灰岩含水层中进行。哥本哈根以西的抽水试验显示了一个裂缝性含水层的实例,该裂缝在井壁对皮肤有明显的负面影响。科威特的Wafra W1流动井在两层含水层中运作,由于泄漏超出了估计半径为2460 m的圆形区域,因此显示出足够的垂直补给。

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  • 来源
    《Ground water》 |2019年第5期|687-692|共6页
  • 作者单位

    Univ Miskolc Fac Earth Sci & Engn Inst Environm Management H-3515 Miskolc Hungary|Bocskai U 13 H-1204 Budapest Hungary;

    Univ Miskolc Fac Earth Sci & Engn Inst Environm Management H-3515 Miskolc Hungary|Univ Miskolc MTA ME Geoengn Res Grp H-3515 Miskolc Hungary;

    Univ Miskolc Fac Earth Sci & Engn Inst Environm Management H-3515 Miskolc Hungary;

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