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首页> 外文期刊>Transport in Porous Media >The Effect of Wettability on Waterflood Oil Recovery in Carbonate Rock Samples: A Systematic Multi-scale Experimental Investigation
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The Effect of Wettability on Waterflood Oil Recovery in Carbonate Rock Samples: A Systematic Multi-scale Experimental Investigation

机译:润湿性对碳酸盐岩样品中水溢油回收的影响:系统多规模实验研究

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摘要

The effect of wettability on waterflooding oil recovery and the associated pore-scale displacement mechanisms are systematically investigated during flow processes in limestone core samples with a broad spectrum of wettability. Using a miniature core-flooding setup integrated with micro-computed tomography (CT) imaging apparatus, we, for the first time, characterize in situ equilibrium wettability states and demonstrate capillary interactions of the flowing phases in strongly water-wet (SWW), intermediate-wet (IW), weakly oil-wet (WOW), and strongly oil-wet (SOW) systems. The microscale observations were then employed to explain the recovery results obtained from replicate, macroscale experiments. The waterflooding parameters, such as experimental temperature, brine composition, defending and invading phase properties, and the initial water saturation, were maintained nearly identical in all of the waterflooding tests, thereby ensuring that the wettability state was the only factor that controlled the variations in waterflood oil recoveries. We provide pore-scale evidences of various pore-scale displacement mechanisms and the consequent fluid configurations in systems with different wettability states. These findings are then linked to the recovery trends of macroscale experiments. The production from IW, WOW, and SOW cases portrayed a prolonged oil recovery owing to the gradual invasion of brine into small and intermediate-sized oil-wet pores. The IW case showed the highest oil recovery among all cases. Moreover, when the injection flow rate was increased, the oil recovery was gradually increased for the IW, WOW, and SOW systems, whereas no significant additional production was observed in the case of SWW.
机译:在具有广泛润湿性的石灰石核心样品中的流动过程中系统地研究了润湿性对水上的润湿性和相关的孔隙级位移机制的影响。使用与微计算机断层扫描(CT)成像装置集成的微型核心泛洪设置,我们首次表征原位平衡润湿性状态,并证明了在强水湿(SWW),中间的流动相的毛细相互作用-WET(IW),弱油(哇)和强烈油湿(母猪)系统。然后采用微观观察来解释从重复,宏观实验获得的回收结果。在所有水上测试试验中,水顶,如实验温度,盐水组合物,防守和入侵相位性能以及初始水饱和度,从而确保润湿状态是控制变化的唯一因素水泡油回收。我们提供各种孔径位移机构的孔隙尺度证据以及具有不同润湿性状态的系统中的随后的流体配置。然后将这些发现与宏观实验的恢复趋势相关联。由于盐水逐渐入侵小型和中等大小的油湿毛孔,从IW,WOW和SOW案例中生产了一段延长的储油。 IW案例显示所有案例中的最高储存。此外,当注射流量增加时,对于IW,WOW和播种系统,逐渐增加了溢油,而在SWW的情况下,没有观察到显着的额外生产。

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