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Comparative analyses of pumping tests conducted in layered rhyolitic volcanic formations

机译:层状流纹质火山岩地层中抽水试验的对比分析

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The rhyolitic volcanic formations are modeled as multilayer flow systems composed of high permeability fractured zones separated by less permeable depth intervals referred to as matrix zones. The multilayer or linear cross flow model is applied which considers lateral flow in all units. The vertical cross flow between the model layers is calculated as the product of the head difference and the vertical inter-layer conductance. The axi-symmetrical well flow simulation software WT (i) applies either analytical or numerical drawdown simulators in the formation, (ii) assumes uniform well bore drawdown conditions in the pumping wells, and (iii) considers drawdown driven induced flow in the observation well. The interpretation of the pumping-recovery test in the well Megyaszo K-9 (Hungary) includes 7 low permeability and 6 screened water yielding zones and applies analytical method to compute the formation response. The benchmark Drill Hole Wash pumping test (Nevada) with pumped and monitoring open boreholes involves-5 fracture and 8 matrix zones. The radial formation heterogeneity is approximated by the bi-zonal flow domain and numerical method is used for drawdown simulation in the formation. Appropriate agreement with the measured drawdown data (both tests) and flow logging data (Drill Hole Wash) is achieved. Computer aided calibration is used for the parameter estimation. The results of the presented evaluations are compared with outputs of independent analyses. (C) 2014 Published by Elsevier B.V.
机译:流纹岩的火山岩层被建模为由高渗透性裂缝带组成的多层流系统,这些裂缝带之间的渗透性较差的深度间隔被称为基质带。应用了多层或线性错流模型,该模型考虑了所有单元中的横向流。模型层之间的垂直横流计算为水头差和垂直层间电导的乘积。轴对称井流模拟软件WT(i)在地层中应用分析或数值降落模拟器,(ii)假设抽水井中井眼的降落条件均匀,并且(iii)考虑到观察井中由降落驱动的感应流。 Megyaszo K-9井(匈牙利)中的抽水-回收测试的解释包括7个低渗透率和6个筛分的产水区,并应用分析方法来计算地层响应。基准抽水钻探抽水测试(内华达州)具有抽水和监测裸眼井孔,涉及5个裂缝和8个基质区域。径向地层非均质性通过双区域流域进行了近似,并且数值方法被用于地层的沉降模拟。与测得的压降数据(两次测试)和流量记录数据(钻孔冲洗)达到适当的一致性。使用计算机辅助校准进行参数估计。提出的评估结果与独立分析的结果进行比较。 (C)2014由Elsevier B.V.发布

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