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Practical Approach to Determine Residual Gas Saturation and Gas-Water RelativePermeability

机译:确定残留气体饱和度和气水相对渗透率的实用方法

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Laboratory measurement of residual saturation (Sgr) in coresamples is a matter of some debate due to the lack of acommonly accepted general method. Different protocols canlead to different values of Sgr being generated, with theassociated uncertainty for simulation input. A previouslyconducted study indicates to the authors that steady-statedisplacement and co-current imbibition are the preferredmethods to generate resevoir representative values of Sgr. Thesteady-state technique is designed to yield full-curve relativepermeability data in addition to Sgr, but it is both costly andtime-consuming. The objective of this paper is to introduce amethod that yields both Sgr and predicted water displacing gasrelative permeability data in a time-effective and cost-effectivemanner.To determine their accuracy, the relative permeabilitycurves derived from this method have been compared to thosefrom actual laboratory test results on core samples fromvarious water-driven gas reservoirs in Australia, New Zealand,SouthEast Asia and the U.S.A. The data predicted using ourmethod have also been compared to relative permeability datapredictions using correlations previously developed by otherresearchers.The data comparisons indicate that relative permeabilitycurves generated using our new (MAK) method not onlycorrelate well with laboratory-measured steady-state curves,but also more closely approximate the laboratory data thatpredictions using previously published methods.
机译:由于缺乏公认的通用方法,实验室对岩心样品中残留饱和度(Sgr)的测量存在争议。不同的协议可能导致生成不同的Sgr值,以及模拟输入的不确定性。先前进行的一项研究向作者指出,稳态位移和并流吸收是生成Sgr的储库代表值的首选方法。除了Sgr之外,稳态技术还可以生成全曲线的相对磁导率数据,但它既昂贵又费时。本文的目的是介绍一种既可生成Sgr值又可预测水驱气相对渗透率数据的方法,该方法既有效又具有成本效益。为了确定其准确性,已将该方法得出的相对渗透率曲线与实际实验室测试中的相对渗透率曲线进行了比较来自澳大利亚,新西兰,东南亚和美国的各种水力驱动气藏的岩心样品的结果也已使用其他方法先前使用相关性将使用我们的方法预测的数据与相对渗透率数据预测进行了比较。数据比较表明,使用我们的新(MAK)方法不仅与实验室测得的稳态曲线具有良好的相关性,而且还可以更精确地近似使用以前发布的方法预测的实验室数据。

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