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Estimation of sub-core permeability statistical properties from coreflooding data

机译:从岩心驱替数据估算子岩心渗透率统计特性

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Knowledge of sub-core permeability is necessary for accurate numerical modeling of coreflooding experiments and for investigation of sub-core flow phenomenon. A new method for estimating sub-core permeability geometric mean (k(G)) and log-permeability variance (sigma(2)(y)) is presented. The method is based on matching coreflooding experiment measurements of wetting phase relative permeability with semi-analytical calculations of effective relative permeability. The semi-analytical solution is formulated assuming log-normal permeability (k), steady state and capillary-limit conditions. It is based on the geometric mean and log-phase-permeability variance for isotropic k and power law averaging for anisotropic correlations. The solution is validated on synthetic k realizations by comparison with numerical calculations. Then, the estimation method is tested on synthetic data assuming various types of core capillary pressure relationships, relative permeability functions and k anisotropies. Results demonstrate high accuracy in almost all of the cases except for small anisotropy ratios l(h)/l(v) between horizontal (l(h)) and vertical (l(v)) dimensionless correlation lengths, where flow is in the horizontal direction, and when sigma(2)(y) is large. The method is also validated using data from CO2-brine coreflooding experiments conducted on two different cores. It is found that the estimation method remains accurate in these realistic settings, however, accuracy of kG is reduced when the core permeability departs from a log-normal distribution. (C) 2017 Elsevier Ltd. All rights reserved.
机译:子岩心渗透性的知识对于岩心驱替实验的精确数值建模和研究子岩心流动现象是必要的。提出了一种估计子岩心渗透率几何平均值(k(G))和对数渗透率方差(sigma(2)(y))的新方法。该方法基于润湿相相对渗透率的岩心驱替实验测量值与有效相对渗透率的半解析计算的匹配。假设对数法向渗透率(k),稳定状态和毛细管极限条件,则配制半分析溶液。它基于各向同性k的几何平均值和对数相渗透率方差,以及各向异性相关性的幂律平均。通过与数值计算进行比较,该解决方案在合成k实现中得到了验证。然后,在假设各种类型的岩心毛细管压力关系,相对渗透率函数和k各向异性的情况下,对合成数据进行测试。结果表明,在几乎所有情况下,除了水平方向(l(h))和垂直方向(l(v))之间的各向异性较小的各向异性比率l(h)/ l(v)以外,几乎所有情况下都具有较高的精度,其中,水平方向上存在流动方向,以及sigma(2)(y)大时。还使用在两个不同岩心上进行的CO2盐水岩心驱替实验的数据验证了该方法。可以发现,在这些实际设置中,估算方法仍然是准确的,但是,当岩心渗透率偏离对数正态分布时,kG的准确性就会降低。 (C)2017 Elsevier Ltd.保留所有权利。

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