利用改进的FZI技术识别巴西盐下储层岩石类型

Nadege Bize Forest, F. Abbots, V. Baines, A. Boyd
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引用次数: 1

摘要

储层岩石类型(RRT)的定义是碳酸盐岩储层评价和表征中的一个关键挑战,这一步至关重要,因为RRT定义了构建3D模型的基本模块,因为RRT定义与静态和动态储层属性有关。本文介绍了一种结合地质和岩石物理性质的创新的协同岩石分型方法,并定制了流动带指示器(FZI)方法,以识别RRT并表征巴西海上Santos盆地的非均质含油盐下碳酸盐岩。利用Barra Velha组盐下碳酸盐岩的448 MICP数据集建立FZI-RRT模型。采用以毛管压力参数、渗透率、有效孔隙度和含水饱和度为输入参数的无监督神经网络,确定了最佳RRTs数量(共5个)。根据岩心的流动特性、测井尺度和EOR处理的适用性,通过10%孔隙度下的FZI值和关键渗透率值来划分这五个类别。这五个RRTs定义了一个独特的渗透率/孔隙度方程,该方程可以传播到整个岩心数据集和测井域。然后为每个RRT创建一个ID卡,其中包含特定的静态和动态属性(孔隙度、渗透率、含水饱和度、相对渗透率),可用于3D油藏建模。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identifying Reservoir Rock Types Using a Modified FZI Technique in the Brazilian Pre-Salt
The definition of Reservoir Rock Types (RRT) is a key challenge in the evaluation and characterization of carbonate reservoirs, and this step is critical as the RRT's define the building blocks for constructing 3D models, as RRT definition links to static and dynamic reservoir properties. This paper describes an innovative and synergetic rock typing process linking geology and petrophysical properties, with a customization of the Flow Zone Indicator (FZI) method to identify RRT's and characterize the heterogeneous oil-bearing Pre-salt carbonates of the Santos Basin, Brazil offshore. A data set of 448 MICP from the Pre-Salt carbonates of Barra Velha Formation was used to build the FZI-RRT model. The optimal number of RRTs, five in total, is determined by using an unsupervised neural network with capillary pressure parameters as inputs, permeability, effective porosity and water saturation. The five classes are delineated by FZI values at 10% porosity and key permeability values, chosen for reasons due flow properties at the core and log scale and suitability in EOR treatments. The five RRTs define a unique permeability/porosity equation that can be propagated to the full core dataset and to the log domain. An ID card for each RRT is then created with specific static and dynamic properties (porosity, permeability, water saturation, relative permeability) that can be used for 3D reservoir modeling.
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