A Novel Approach for Estimating Formation Permeability in a Highly Heterogeneous Reservoir in Middle East

R. Celma, A. Lavenu
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Abstract

Estimating flow in the reservoir is critical for production forecasting, 3D modeling and field development. Laboratory experiments are the main source of information for the permeability, but the results might be impacted by a high degree of reservoir heterogeneity, as well as by the upscaling from core to log. The studied reservoir displays a complex lithology — limestone and dolomite – where dolomitization appears to be a clear reservoir rock quality enhancer. High permeability streaks can be related to dolomitized intervals, however a simple porosity vs. permeability function cannot capture the large variation of this property (from 0.1 to 5000mD) In this study, the volumetrics computed from a comprehensive petrophysical model that includes the integration of core descriptions, XRD, and gamma ray spectroscopy to properly estimate the fractions of limestone, dolomite, clay, and heavy minerals were used. A core to log correlation was made and it clearly showed how the dolomitization improves our reservoir properties, in particular the permeability. Trends functions were established based on the stratigraphy and on the content of limestone/dolomite. These trends were used to train a fuzzy logic model supported by other logs such as: normalized porosity and density-neutron vector angle/length. The vector angle/length are coordinate transforms to convert neutron density into linear independent vectors. This approach addresses the large variation of permeability related to the strong diagenetic footprint onto the reservoir. The results were compared to permeability from core and KH from PTA analysis, and displayed an error of less than 5%
中东地区高非均质油藏储层渗透率估算新方法
储层流量估算对于产量预测、三维建模和油田开发至关重要。实验室实验是渗透率的主要信息来源,但结果可能受到储层高度非均质性以及从岩心到测井的升级的影响。研究的储层岩性复杂,为灰岩和白云岩,其中白云化作用明显增强了储层岩石质量。高渗透条纹可能与白云化层段有关,但简单的孔隙度与渗透率函数无法捕捉该属性的大变化(从0.1到5000mD)。在本研究中,通过综合岩石物理模型计算出的体积,包括岩心描述、XRD和伽马射线能谱的整合,以正确估计石灰岩、白云岩、粘土和重矿物的组分。岩心与测井对比清楚地显示了白云化如何改善储层性质,特别是渗透率。建立了基于地层和灰岩/白云岩含量的趋势函数。这些趋势被用来训练一个由其他测井数据支持的模糊逻辑模型,如:归一化孔隙度和密度-中子矢量角/长度。矢量角/长度进行坐标变换,将中子密度转换为线性独立矢量。这种方法解决了与储层上的强成岩足迹有关的渗透率的巨大变化。结果与岩心渗透率和PTA分析的KH进行了比较,误差小于5%
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