Determination of Reservoir Hydraulic Flow Units and Permeability Estimation Using Flow Zone Indicator Method

Alyaa M. Ali, Ayad A. Alhaleem
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Abstract

   Reservoir characterization plays a crucial role in comprehending the distribution of formation properties and fluids within heterogeneous reservoirs. This knowledge is instrumental in constructing an accurate three-dimensional model of the reservoir, facilitating predictions regarding porosity, permeability, and fluid flow distribution. Among the various methods employed for reservoir characterization, the hydraulic flow unit stands out as a widely adopted approach. By effectively subdividing the reservoir into distinct zones, each characterized by unique petrophysical and geological properties, hydraulic flow units enable comprehensive reservoir analysis. The concept of the flow unit is closely tied to the flow zone indicator, a critical parameter that defines the porosity-permeability relationships of each hydraulic flow unit. Additionally, the flow zone indicator method proves valuable in estimating permeability accurately. In this study, we demonstrate the application of the flow zone indicator method to determine hydraulic flow units within the Khasib formation. By analyzing core data and calculating the Rock Quality Index (RQI) and Flow Zone Indicator (∅Z), we differentiate the formation into four hydraulic flow units based on FZI values. Specifically, HFU 1 represents a rock of poor quality, corresponding to compact and chalky limestone. HFU 2 represents intermediate quality, corresponding to argillaceous limestone, while HFU 3 represents good quality, corresponding to porous limestone. Lastly, HFU 4 signifies an excellent reservoir rock quality characterized by vuggy limestone. By establishing a permeability equation that correlates with effective porosity for each rock type, we successfully estimate permeability. Comparing these estimated permeability values with core permeability reveals a strong agreement with a high correlation coefficient of 0.96%. Consequently, the flow zone indicator method effectively classifies the Khasib formation into four distinct hydraulic flow units and provides an accurate and reliable means of determining permeability in the reservoir. The resulting permeability equations can be applied to wells and depth intervals lacking core measurements, further emphasizing the practical utility of the FZI method.
用流动区指标法确定油藏水力流动单元及渗透率
储层表征在理解非均质储层中的地层性质和流体分布方面起着至关重要的作用。这些知识有助于构建准确的储层三维模型,有助于预测孔隙度、渗透率和流体流量分布。在储层表征所采用的各种方法中,水力流动单元是一种被广泛采用的方法。通过有效地将储层细分为不同的区域,每个区域都具有独特的岩石物理和地质特性,水力流动单元能够进行全面的储层分析。流动单元的概念与流动区指示器密切相关,流动区指示器是定义每个水力流动单元的孔隙度-渗透率关系的关键参数。此外,流动区指示法在准确估计渗透率方面也证明了其价值。在本研究中,我们展示了流动区指示器方法在确定Khasib地层内水力流动单元方面的应用。通过分析岩心数据并计算岩石质量指数(RQI)和流动区指标(∅Z),我们根据FZI值将地层区分为四个水力流动单元。具体而言,HFU 1代表质量较差的岩石,对应于致密的白垩质石灰岩。HFU 2代表中等质量,对应泥质石灰岩,而HFU 3代表良好质量,对应多孔石灰岩。最后,HFU 4表示储层岩石质量优良,其特征为溶洞状石灰岩。通过建立与每种岩石类型的有效孔隙度相关的渗透率方程,我们成功地估计了渗透率。将这些估计的渗透率值与岩心渗透率进行比较,显示出很强的一致性,相关系数高达0.96%。因此,流动带指标法有效地将Khasib地层划分为四个不同的水力流动单元,并为确定储层渗透率提供了一种准确可靠的方法。所得渗透率方程可应用于缺乏岩心测量的井和深度层段,进一步强调了FZI方法的实用性。
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