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Flow units and rock type for reservoir characterization in carbonate reservoir case study, south of Iraq

机译:碳酸盐储层案例研究中的流量单位和岩型,伊拉克南部

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The current work is focused on the rock typing and flow unit classification for reservoir characterization in carbonate reservoir, a Yamama Reservoir in south of Iraq (Ratawi Field) has been selected, and the study is depending on the logs and cores data from five wells which penetrate Yamama formation. Yamama Reservoir was divided into twenty flow units and rock types, depending on the Microfacies and Electrofacies Character, the well logs pattern, Porosity–Water saturation relationship, flow zone indicator (FZI) method, capillary pressure analysis, and Porosity–Permeability relationship (R35) and cluster analysis method. Four rock types and groups have been identified in the Yamama formation depending on the FZI method, where the first group represents the bad reservoir quality (FZI-1) (Mudstone Microfacies and Foraminiferal wackestone Microfacies), the second group reflects a moderate quality of reservoir (FZI-2) (Algal wackestone–Packstone Microfacies and Bioclastic wackestone–Packstone Microfacies), the third group represents good reservoir quality (FZI-3) (Peloidal Packstone–Grainstone Microfacies), and the fourth group represents a very good reservoir quality (FZI-4) (Peloidal–oolitic Grainstone Microfacies). Capillary pressure curves and cluster analysis methods show four different rock types: a very good quality of reservoir and porous (Mega port type) (FZI-4) (Peloidal–oolitic Grainstone Microfacies) with a low irreducible Water saturation (Swi), good quality of reservoir and porous (Macro port type) (FZI-3) (Peloidal Packstone–Grainstone Microfacies), moderate quality of reservoir (Meso port type) (FZI-2) (Algal wackestone–Packstone Microfacies and Bioclastic wackestone–Packstone Microfacies), and a very fine-grained with bad reservoir quality (Micro port type) (FZI-1) (Mudstone Microfacies and Foraminiferal wackestone Microfacies) and with the higher displacement of pressure). These capillary pressure curves support the subdivision of the main reservoir unit to flow units.
机译:目前的工作主要集中在碳酸盐储层中的岩石打字和流量单位分类,伊拉克南部(Ratawi Field)中的山马水库已经选择,研究取决于来自五个井的日志和核心数据穿透山马形成。 Yamama水库分为二十个流量单位和岩石类型,取决于微缩流和电涂层特征,井原木图案,孔隙率 - 水饱和关系,流量区指示器(FZI)方法,毛细管压力分析和孔隙率渗透性关系(R35 )和聚类分析方法。在山马形成中确定了四种岩石类型和群体,这取决于FZI方法,其中第一组代表储层质量不好(FZI-1)(泥岩微缩法和面孔疣微缩胶质胶质胶质胶质胶质胶质胶质胶质胶质胶质剂),第二组反映了适度的水库质量(FZI-2)(藻类瓦斯托酮 - 包装石微型胶囊和生物塑料瓦斯通 - 包装微电缩放),第三组代表良好的储层质量(FZI-3)(Peloidal Propstone-graillstone Microfacies),第四组代表了一个非常好的储层质量( FZI-4)(Peloidal-oolitic Streagstone Microfacies)。毛细管压力曲线和簇分析方法显示出四种不同的岩石类型:具有较低不可缩小的水饱和度(SWI),质量优良的水库和多孔(兆口型)(FZI-4)(FZI-4)(FZI-4)(Peloider-4)(SWI),质量好储层和多孔(宏观点)(FZI-3)(FZI-3)(Peloidal Packstone - 晶石微缩醛),适度的水库(Meso Port Type)(FZI-2)(藻类 - 瓦斯托通 - 包装微电容和生物弹性Wackestone - Packstone Microfacies),和储层质量不好(微口型)(FZI-1)(FZI-1)(泥岩微缩醛和面包丝疣微缩放)非常细粒度,具有较高的压力位移)。这些毛细管压力曲线支撑主储存器单元的细分流动单元。

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