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首页> 外文期刊>Journal of Petroleum Science & Engineering >Effects of pore geometry and rock properties on water saturation of a carbonate reservoir
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Effects of pore geometry and rock properties on water saturation of a carbonate reservoir

机译:孔隙结构和岩石性质对碳酸盐岩储层含水饱和度的影响

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摘要

Capillary pressure analysis is an important piece of every reservoir rock study. Mercury injection capillary pressure (MICP) is one of the best methods for pore geometry analysis among different techniques for obtaining the capillary pressure data. Pore-facies analysis is a useful method for classifying the carbonate reservoir rocks directly according to their pore system characteristics using the MICP curves. One of the challenging subjects in every carbonate reservoir study is the characterization of reservoir fluids behavior in the pore network. The purpose of this study is determining the effect of the rock properties and pore geometry on water saturation in the carbonate reservoir rocks. Two types of reservoir rock classification were performed based on the MICP and air-water capillary pressure data. The results show that the reservoir rock samples with specific depositional texture, pore type and cement content show distinct capillary and water saturation behavior. Therefore, the pore geometry of rock samples has a strong effect on the fluid movements and entrapment in the reservoir rock. In turn, it is the result of depositional texture and diagenetic features. Although understanding the relationship between the rock properties and capillary behavior and determining the controlling parameters in fluid behavior in the pore network is very difficult and time consuming in carbonate reservoirs with such a complicated pore system, it is possible by detailed capillary pressure and petrographic studies.
机译:毛细管压力分析是每个储层岩石研究的重要组成部分。在获得毛细压力数据的不同技术中,注汞毛细压力(MICP)是进行孔几何分析的最佳方法之一。孔隙相分析是使用MICP曲线根据孔隙系统特征直接分类碳酸盐岩储层岩石的有用方法。每个碳酸盐储层研究中具有挑战性的主题之一是表征孔隙网络中储层流体的行为。这项研究的目的是确定岩石性质和孔隙几何形状对碳酸盐岩储集层中水饱和度的影响。基于MICP和空气-水毛细管压力数据进行了两种类型的储集岩分类。结果表明,具有特定沉积质地,孔隙类型和水泥含量的储层岩石样品表现出明显的毛细作用和水饱和行为。因此,岩石样品的孔隙几何形状对储层岩石中的流体运动和截留有很大的影响。反过来,这是沉积质地和成岩特征的结果。在具有如此复杂孔隙系统的碳酸盐岩油藏中,尽管了解岩石性质与毛细管行为之间的关系并确定孔隙网络中流体行为的控制参数非常困难且耗时,但通过详细的毛细管压力和岩石学研究还是可能的。

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