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REVIEW OF THE INTERCEPT METHOD FOR RELATIVE PERMEABILITY CORRECTION USING A VARIETY OF CASE STUDY DATA

机译:使用各种案例研究数据审查相对渗透校正的截距方法

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In 2014,Gupta and Maloney1 introduced a novel method of measuring steady state relative permeability,called the Intercept Method. The Intercept Method entails a modification of a standard steady state procedure that incorporates multiple total flow rates at each fractional flow rate. The objective of the method is to measure data at each fractional flow rate that will permit simple analytical calculations to correct differential pressure(hence relative permeability)and saturation data for the effects of capillary pressure. The Intercept Method is intended to provide a corrective technique without the need for additional supportive analyses,such as capillary pressure and in situ saturation monitoring(ISSM),or as an alternative approach to the current considered best practice of numerical coreflood simulation,which generally requires the specified additional data. Consequently,the Intercept Method is of interest to the global industry in regions and/or laboratories that do not possess state-of-the-art equipment,or for its cost saving potential. However,before employing this new method,it was important to the authors to investigate its validity across the range of rock properties,sample dimensions and wettabilities experienced in commercial SCAL coreflood experiments. This study thus draws on a variety of relative permeability curves(and supporting data)from various global core studies,originally derived by typical relative permeability methods plus coreflood simulation. From these data,we use SCORES to simulate the expected results of multi-flowrate steady state experiments and use the Intercept Method to derive and compare the corrected relative permeability curves. Results highlight criteria under which the method does not provide fully corrected data. The paper explores these criteria in more detail.
机译:2014年,Gupta和Maloney1介绍了一种衡量稳态相对渗透率的新方法,称为截距方法。截距方法需要修改标准稳态步骤,该方法包含多个分数流量的多个总流速。该方法的目的是测量每个分数流速的数据,这将允许简单的分析计算来校正毛细管压力的差分压力(因此相对渗透率)和饱和数据。截距方法旨在提供纠正技术,而无需额外的支持性分析,例如毛细管压力和原位饱和监测(ISSM),或者作为当前考虑的最佳实践的替代方法通常需要指定的附加数据。因此,拦截方法对全球产业的地区和/或实验室中没有最先进的设备或成本节约的潜力感兴趣。然而,在采用这种新方法之前,作者对作者来说,在商业尺度内核实验中经历的岩石属性,样本尺寸和湿润范围内调查其有效性。因此,本研究借鉴了各种全局核心研究的各种相对渗透性曲线(和支持数据),最初由典型的相对渗透方法加上CoreFlood模拟来实现。根据这些数据,我们使用分数来模拟多流量稳态实验的预期结果,并使用截距方法导出并比较校正的相对磁导曲线。结果突出显示该方法未提供完全校正的数据的标准。本文更详细地探讨了这些标准。

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