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A New Method to Calculate Effective Permeability of a Naturally Fractured Carbonate Reservoir from Seismic Attributes

机译:一种计算自然裂缝碳酸盐储层从地震属性的有效渗透性的新方法

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Modeling permeability of naturally fractured reservoirs for simulation studies and field development planning is very challenging since the data required for characterizing the magnitude and distribution of reservoir fracture permeability is veiy limited. Fracture permeability is traditionally measured from cores and/or estimated from well tests. These estimations usually work adequately at well locations for permeability modeling but poorly between wells. Modeling fracture permeability distribution between wells and/or away from wells is a very important step to build a reliable reservoir simulation model for business needs. This paper presents a new method/workflow for modeling effective permeability of a naturally fractured carbonate reservoir from seismic attributes. The new method directly converts fracture textures and distributions from seismic attributes into permeability for reservoir simulation. Core and log data are used to create fracture regions and the distribution of fracture density; well test data are applied to generate isotropic permeability; and seismic attributes (e.g., ant-tracks, curvature, and anisotropy) are utilized to model the fracture network and permeability anisotropy. New equations are created to calculate effective permeability of the reservoir by scaling up and down between core/well test and seismic data. Two history match parameters (fracture network connectivity and permeability anisotropy) are introduced to assist the history match process within the guidance of seismic and geologic data. The new method/workflow has been successfully applied to solve the history match challenges of a naturally fractured reservoir in a Middle Eastern field for which no history matched model was achieved before. Applying the new method has significantly improved water movement matches in all producers of the field.
机译:自然裂缝储层的模拟研究和现场开发规划的建模渗透性是非常具有挑战性,因为表征储层骨折渗透率的幅度和分布所需的数据是Veiy Limited。骨折渗透性传统上从核心测量和/或从井测试中估计。这些估计通常在孔隙位置的井位置充分工作,但在井之间差不多。井和/或远离井间的裂缝渗透性分布是一个非常重要的步骤,为业务需求建立可靠的水库仿真模型。本文介绍了一种新的方法/工作流程,用于从地震属性对天然碎屑储层的有效渗透性进行建模。新方法直接从地震纹理和分布转换为储层模拟的渗透率。核心和日志数据用于产生骨折区域和断裂密度的分布;良好的测试数据用于产生各向同性渗透性;和地震属性(例如,蚂蚁轨道,曲率和各向异性)用于模拟裂缝网络和渗透性各向异性。创建了新的方程,以通过在核心/井测试和地震数据之间上下缩放来计算水库的有效渗透性。引入了两个历史匹配参数(断裂网络连接和渗透性各向异性),以帮助历史匹配过程在地震和地质数据的指导中。新的方法/工作流程已成功应用于解决自然破碎储层在中东领域的历史匹配挑战,以前没有历史匹配模型。应用新方法在田地的所有生产商中具有显着改善的水运动比赛。

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