塔里木盆地碳酸盐岩岩溶储层岩溶裂缝分层建模方法

F. Shen, Kuanzhi Zhao, Yintao Zhang, Y. Yu, Jingliang Li
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引用次数: 2

摘要

塔里木盆地岩溶储层是由奥陶系的陆上暴露和岩溶作用形成的,代表了主要的储层。预测储层容量和量化渗透率非均质性对油田开发规划具有重要的挑战性。在本文中,我们提出了一种利用地球科学和工程数据对岩溶和裂缝进行分层建模的方法,用于选择新井的位置和油藏模拟。多尺度的岩溶和裂缝对储层体积和油井产能有重要影响。利用基于测井的电相,结合岩心数据、图像测井和钻井数据进行验证,确定井中的裂缝-岩溶单元,以量化单元中不同的岩溶特征和裂缝模式。基于多属性地震相分析,利用提取的地震尺度岩溶特征,构建了岩溶系统的三维建筑模型。利用井内岩溶裂缝单元、反演地震阻抗体和三维岩溶构造模型建立岩溶网络模型。利用测井资料、泥浆损失资料、地震阻抗体积和岩溶网络模型对岩溶系统孔隙度进行估算。建立了岩溶水平和垂直管道模型,并对其渗透率进行了经验推导。根据裂缝长度与地震分辨率的关系,在两个尺度上对裂缝进行建模。以图像测井资料和岩溶裂缝单元模型为随机条件,建立了小尺度弥漫性裂缝模型。根据曲率增强属性自动跟踪裂缝轮廓,对裂缝进行网格划分,确定地建立了大尺度离散裂缝网络模型。DFN模型被嵌入到geocell网格模型中,该模型明确地保持了大裂缝的几何形状。裂缝体系有效水平和垂直渗透率的计算是尺度相关且解耦的。根据试井数据校准裂缝几何参数和渗透率。在静态模型中进行流线模拟,以校准空间裂缝密度。经过两步调节后,更新裂缝模型,然后进行升级。根据岩溶和裂缝对流体流动的影响,将其从井筒到地震尺度的流动特性结合起来。利用流线模拟将岩溶网络模型与含水率和井底压力的历史匹配相结合,有助于油水接触面(OWC)评价和动态隔室的识别。结合岩溶网络、动态隔层和模拟地质情景,可以瞄准潜在的高产区,选择新的井位。案例研究表明,采用分层方法对岩溶和裂缝进行建模和校准,可以建立真实的储层模型,更好地了解储层的复杂性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hierarchical Approach to Modeling Karst and Fractures in Carbonate Karst Reservoirs in the Tarim Basin
Karst reservoirs in the Tarim Basin, northwestern China, were formed by subaerial exposure and karstification from the Ordovician formation and represent the main plays. Predicting the storage capacity and quantifying permeability heterogeneities are challenging while important for field development planning. In this paper we present a hierarchical approach to modeling karst and fractures with geoscience and engineering data for selecting locations of new wells and for the reservoir simulation. Karst and fractures at multiple scales contribute significantly to reservoir volumes in place and well productivity. Fracture-karst units in wells were determined using log-based electrofacies validated against core data, image logs and drilling data to quantify different karst features and fracture patterns hosted in units. A 3-D architecture model of karst system was constructed with extracted karst features at the seismic-scale based on multi-attribute seismic facies analysis. The karst network model was generated with karst-fracture units at wells, inverted seismic impedance volume, and 3-D karst architecture model. Porosity estimates of the karst system were conditioned with log data, mud loss data, seismic impedance volume and karst network model. Karst horizontal and vertical conduits were modeled and their permeabilities were empirically derived. Based on fracture length relative to the seismic resolution, fractures were modeled at two scales. Diffuse fractures at a small scale were modeled stochastically conditioned with image log data and the karst fracture unit model. A discrete fracture network (DFN) model at a large scale was deterministically built by meshing fracture lineaments automatically tracked from the curvature enhanced attribute. The DFN model was embedded into a geocellular grid model in which geometries of the large fractures were maintained explicitly. The calculation of effective horizontal and vertical permeabilities of the fracture system was scale dependent and decoupled. Fracture geometric parameters and permeabilities were calibrated against well test data. Streamline simulation was performed in the static model to calibrate spatial fracture densities. After two-step conditioning, fracture models were updated and then upscaled. Flow properties of karst and fractures from the wellbore to the seismic scales were combined based on their impacts on fluid flow. Integration of karst network model and history match of water cut and bottom hole pressure using streamline simulation helped the oil/water contact (OWC) assessment and allowed the identification of dynamic compartments. Combing karst networks, dynamic compartments and modeled geological scenarios allowed targeting potential highly productive zones where new well locations could be selected. The case study demonstrated that the hierarchical approach to karst and fracture modeling and calibration allowed building a realistic reservoir model and better understanding of the reservoir complexity.
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