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Novel insights into pore-scale dynamics of wettability alteration during low salinity waterflooding

机译:低盐度注水过程中润湿性变化的孔隙尺度动力学的新见解

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摘要

Low salinity waterflooding has proven to accelerate oil production at core and field scales. Wettability alteration from a more oil-wetting to a more water-wetting condition has been established as one of the most notable effects of low salinity waterflooding. To induce the wettability alteration, low salinity water should be transported to come in contact with the oil-water interfaces. Transport under two-phase flow conditions can be highly influenced by fluids topology that creates connected pathways as well as dead-end regions. It is known that under two-phase flow conditions, the pore space filled by a fluid can be split into flowing (connected pathways) and stagnant (deadend) regions due to fluids topology. Transport in flowing regions is advection controlled and transport in stagnant regions is predominantly diffusion controlled. To understand the full picture of wettability alteration of a rock by injection of low salinity water, it is important to know i) how the injected low salinity water displaces and mixes with the high salinity water, ii) how continuous wettability alteration impacts the redistribution of two immiscible fluids and (ii) role of hydrodynamic transport and mixing between the low salinity water and the formation brine (high salinity water) in wettability alteration. To address these two issues, computational fluid dynamic simulations of coupled dynamic two-phase flow, hydrodynamic transport and wettability alteration in a 2D domain were carried out using the volume of fluid method. The numerical simulations show that when low salinity water was injected, the formation brine (high salinity water) was swept out from the flowing regions by advection. However, the formation brine residing in stagnant regions was diffused very slowly to the low salinity water. The presence of formation brine in stagnant regions created heterogeneous wettability conditions at the pore scale, which led to remarkable two-phase flow dynamics and internal redistribution of oil, which is referred to as the "pull-push" behaviour and has not been addressed before in the literature. Our simulation results imply that the presence of stagnant regions in the tertiary oil recovery impedes the potential of wettability alteration for additional oil recovery. Hence, it would be favorable to inject low salinity water from the beginning of waterflooding to avoid stagnant saturation. We also observed that oil ganglia size was reduced under tertiary mode of low salinity waterflooding compared to the high salinity waterflooding.
机译:事实证明,低盐度注水可以在核心和油田规模上加速石油生产。从低油润湿到高水润湿的润湿性改变已被确定为低盐度注水的最显着效果之一。为了引起可湿性改变,应输送低盐度水使其与油水界面接触。在两相流条件下的运输会受到流体拓扑的极大影响,该拓扑会创建连通的通道以及死角区域。众所周知,在两相流动条件下,由于流体的拓扑结构,被流体填充的孔隙空间可以分为流动(连接的路径)和停滞(死角)区域。流动区域中的运输受平流控制,停滞区域中的运输主要受扩散控制。要了解通过注入低盐度水对岩石的润湿性变化的全貌,重要的是要知道i)注入的低盐度水如何置换并与高盐度水混合,ii)连续的润湿性变化如何影响岩石的重新分布。两种不混溶的流体,以及(ii)在润湿性变化中低盐度水与地层盐水(高盐度水)之间的流体动力传输和混合作用。为了解决这两个问题,使用体积法在二维域内进行了耦合动态两相流,流体动力传输和润湿性变化的计算流体动力学模拟。数值模拟表明,注入低盐度水时,通过平流将地层盐水(高盐度水)从流动区域中清除了。但是,停滞区域中的地层盐水非常缓慢地扩散到低盐度水中。停滞区域中地层盐水的存在在孔隙尺度上造成了非均质的润湿性条件,这导致了显着的两相流动力学和油的内部重新分布,这被称为“拉-推”行为,以前没有得到解决。在文学中。我们的模拟结果表明,三次采油中停滞区域的存在阻碍了润湿性改变的可能性,从而增加了采油量。因此,从注水开始就注入低盐度水以避免饱和饱和是有利的。我们还观察到,与高盐度注水相比,在低盐度注水的三级模式下油性神经节大小减小了。

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