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Three-Dimensional Aquifer Heterogeneity in Pumping Test Analysis. A Numerical Investigation Using Radial Flow Models.ud

机译:抽水试验分析中的三维含水层非均质性。使用径向流模型的数值研究。 ud

摘要

Pumping test results are often analysed on the assumption of radial symmetry. This may be becauseudanalytical solutions are used, which are limited to two-dimensional problems, or because of theudwidespread acceptance that this assumption is satisfactory when estimating average values of the aquiferudhydraulic characteristics. A three-dimensional R-θ-Z model, built using an object-oriented approach, isudused to investigate the effects of spatial heterogeneity on time-drawdown curves. Particular attention isudpaid to the variation of aquifer properties in the circumferential direction, a factor ignored in most pumpingudtest analyses.udThe mechanisms in the numerical model include a logarithmically increasing mesh spacing in the radialuddirection, features operating at the pumped borehole and a moving water table. The model is applied toudtwo and three-dimensional idealised aquifers to establish the impact of aquifer heterogeneity. Threedimensionaludaquifer heterogeneity is shown to produce time-drawdown curves that can be matched usingudtwo-dimensional numerical models, giving a misleading interpretation of the aquifer flow processes. Forudexample, a delayed response to pumping at an observation borehole due to a combination of low radialudpermeability and a fracture in the circumferential direction can be mistaken for large aquifer storage whenudradial symmetry is assumed. A field example is presented where this mechanism is believed to operate.
机译:抽水测试结果通常是在径向对称的假设下进行分析的。这可能是因为使用了 uu分析解决方案,该解决方案仅限于二维问题,或者由于 u u n广泛接受了在估算含水层/渗水特征的平均值时该假设令人满意的假设。使用面向对象的方法建立的三维R-θ-Z模型用于研究空间异质性对时间下降曲线的影响。尤其要注意含水层特性在圆周方向上的变化,这是大多数抽水试验中忽略的一个因素。在数值模型中,机理包括沿对数方向对数增加的网格间距,在抽水条件下运行的特征钻孔和移动的地下水位。该模型应用于二维和三维理想含水层,以建立含水层非均质性的影响。三维非水样层的非均质性显示出可以使用二维数值模型来匹配的时间下降曲线,从而对含水层流动过程产生了误导性的解释。例如,假定径向对称时,由于径向渗透率低和周向裂缝的组合而导致的对观测井眼泵水的延迟响应可能被误认为储层较大。给出了一个实例,据信该机制可以运行。

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