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Imaging and Measurement of Pore-Scale Interfacial Curvature to Determine Capillary Pressure Simultaneously With Relative Permeability

机译:成像和测量孔隙度界面曲率,同时测定相对渗透率的毛细血管压力

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摘要

There are a number of challenges associated with the determination of relative permeability and capillary pressure. It is difficult to measure both parameters simultaneously on the same sample using conventional methods. Instead, separate measurements are made on different samples, usually with different flooding protocols. Hence, it is not certain that the pore structure and displacement processes used to determine relative permeability are the same as those when capillary pressure was measured. Moreover, at present, we do not use pore-scale information from high-resolution imaging to inform multiphase flow properties directly. We introduce a method using pore-scale imaging to determine capillary pressure from local interfacial curvature. This, in combination with pressure drop measurements, allows both relative permeabilities and capillary pressure to be determined during steady state coinjection of two phases through the core. A steady state waterflood experiment was performed in a Bentheimer sandstone, where decalin and brine were simultaneously injected through the core at increasing brine fractional flows from 0 to 1. The local saturation and the curvature of the oil-brine interface were determined. Using the Young-Laplace law, the curvature was related to a local capillary pressure. There was a detectable gradient in both saturation and capillary pressure along the flow direction. The relative permeability was determined from the experimentally measured pressure drop and average saturation obtained by imaging. An analytical correction to the brine relative permeability could be made using the capillary pressure gradient. The results for both relative permeability and capillary pressure are consistent with previous literature measurements on larger samples.
机译:确定相对渗透率和毛细压力存在许多挑战。使用常规方法很难在同一样品上同时测量两个参数。取而代之的是,通常在不同的淹没方案下,对不同的样本进行单独的测量。因此,不确定用于确定相对渗透率的孔结构和位移过程与测量毛细管压力时的孔结构和位移过程相同。此外,目前,我们还没有使用高分辨率成像中的孔隙尺度信息直接告知多相流动特性。我们介绍了一种使用孔隙尺度成像从局部界面曲率确定毛细管压力的方法。结合压降测量,可以在通过芯体的两相稳态共注入过程中确定相对渗透率和毛细管压力。在本特海默(Bentheimer)砂岩中进行了稳态注水实验,其中萘烷和盐水以从0到1的盐水分流增加的方式同时通过岩心注入。确定了油饱和度和油盐水界面的曲率。使用杨-拉普拉斯定律,曲率与局部毛细管压力有关。沿流动方向,饱和压力和毛细管压力均存在可检测到的梯度。相对渗透率由实验测量的压降和通过成像获得的平均饱和度确定。可以使用毛细管压力梯度对盐水的相对渗透率进行分析校正。相对渗透率和毛细压力的结果与以前关于较大样品的文献测量结果一致。

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