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Applications of the Normalized Pore Throat Radius Methodology for Improved Hydraulic Flow Unit Characterization Using the Niger Delta Field as Case Study

机译:标准化孔隙桡骨半径方法的应用,采用尼日尔三角洲领域改进液压流动单元表征的案例研究

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The relation between porosity, permeability and pore architecture in complex reservoir units, typical of the thin bedded canyon turbidite system within the clastic reservoir rocks is complicated and indistinct. The sedimentary architecture usually overprinted by late diagenesis results in the intrinsic complexities which pose major problems in modelling these systems. Detailed assessment of flow units is essential for a better understanding of the reservoir flow behavior and relation between storage and flow capacity. These units are zones composed of similar rock types that are in hydrodynamic communication, which possess stratigraphic continuity and have a strong relationship to pore geometries and rock type, but may not correspond exactly with the depositional facies. This paper presents the application of the normalized pore throat radius ( R_(tot)) methodology for improved hydraulic flow units characterization and production optimization in complex reservoir systems. A modification of the reservoir quality indicator (RQI), Stratigraphic Modified Lorenz Plot (SMLP) and Leverett J-Function methodologies for hydraulic flow unit characterization using the R_(tot) concept demonstrates improved calculation of hydraulic flow units using dataset from the Niger Delta deep water turbiditic system. Results of the analysis for the various genetic reservoir units demonstrate an improvement of 60% over existing methodologies with additional capability for delineating between zones with excellent high communicationand baffles. In addition, Correlation between the irreducible water saturation from mercury injection capillary pressures and FZI presents an improved efficacy of the R_(tot) model for hydraulic flow zone characterization.
机译:在复杂的储层单元,典型的碎屑储集岩中的薄层状峡谷浊系统的孔隙度,渗透率和孔结构之间的关系是复杂的和模糊的。沉积体系结构通常可以通过在构成建模这些系统主要问题的内在复杂晚成岩结果套印。流动单元的详细评估是为了更好地理解存储和流容量之间的储层流动行为和关系是至关重要的。这些单元是相似的岩石类型,可在液力连通,其具有地层连续性并具有孔隙的几何形状和岩石类型牢固的关系构成的区域,但可以不与沉积相精确地对应。本文介绍了归一化的孔喉半径的应用(R_(TOT))的方法在复杂的贮存体系改进的液压流单元表征和生产优化。储层质量指示符(RQI)的修改,地层改性洛伦茨拓扑(SMLP)和使用该R_(TOT)的液压流单元表征概念表现出改进的使用数据集从尼日尔三角洲深液压流单元的计算莱弗里特J-功能的方法水浊积系统。分析的各种遗传储层单元的结果表明,60%以上的现有方法具有附加能力的改善具有优良的高communicationand挡板区之间划定。此外,从汞注入毛细管压力和FZI束缚水饱和度之间的相关性呈现R_(TOT)模型液压流区表征的改进的效力。

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