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Thermodynamic Modeling of Brine Dilution-Dependent Recovery in Carbonate Rocks with Different Mineralogical Content

机译:不同矿物含量的碳酸盐岩中盐水稀释依赖性回收率的热力学模型

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摘要

Extensive experimental studies during the last two decades have demonstrated improved oil recoveries through the injection of diluted brine in both sandstone and carbonate rocks. However, the mechanisms that lead to improved oil recovery in carbonate rocks are not well established, though wettability alteration has been widely cited as a primary mechanism. It is also important to understand the role of carbonate mineralogical composition during diluted brine injection on the geochemical interactions taken place. In this study, we have formulated a theory for the anticipated chemical interactions between oil, brine, and rock, and linked the geochemical interactions to multicomponent transport within the porous rock. In so doing, we investigated different hypotheses on the viable link between geochemical interactions and wettability modifications. Our simulation results could capture the trend in the experimental oil recovery and pressure differential results, together with the effluent ions and pH under varying mineralogical content. On the basis of our model, we infer that mineral alteration alone could not describe the observed behavior and that one has also to consider the interplay between surface charge and mineral alteration. We then followed with simulation of a quarter of a five-spot pattern to demonstrate that incremental recovery varied with different rock mineralogy. The outcomes of our study clearly highlight the need to establish the relationship between appropriate process mechanism(s) and impact of mineralogical content when implementing brine dilution-dependent oil recovery in carbonate reservoirs.
机译:在过去的二十年中,广泛的实验研究表明,通过在砂岩和碳酸盐岩中注入稀盐水,可以提高石油采收率。然而,尽管润湿性改变已被广泛认为是主要机制,但改善碳酸盐岩中石油采收率的机制尚不十分清楚。了解稀释盐水注入过程中碳酸盐矿物组成对发生的地球化学相互作用的作用也很重要。在这项研究中,我们为油,盐水和岩石之间的预期化学相互作用建立了理论,并将地球化学相互作用与多孔岩石中的多组分传输联系起来。通过这样做,我们研究了地球化学相互作用与润湿性修饰之间可行联系的不同假设。我们的模拟结果可以捕获实验油回收率和压差结果的趋势,以及在不同矿物含量下的流出离子和pH值。根据我们的模型,我们推断,仅矿物蚀变不能描述观察到的行为,还必须考虑表面电荷与矿物蚀变之间的相互作用。然后,我们模拟了一个五点模式的四分之一,以证明增量采收率随岩石矿物学的不同而变化。我们的研究结果清楚地表明,在碳酸盐岩储层中进行盐水稀释相关的采油过程时,需要建立适当的处理机制与矿物含量影响之间的关系。

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