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Vug Characterization and Pore Volume Compressibility for Numerical Simulation of Vuggy and Fractured Carbonate Reservoirs

机译:孔隙和裂缝性碳酸盐岩储层数值模拟的孔隙特征和孔隙体积可压缩性

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Three porosity types, matrix, vugs and fractures, are usually present in naturally fractured, vuggy carbonate reservoirs. The vugs are generally considered connected either to the matrix or to the fractures in numerical simulation. One of the challenges of modeling these reservoirs is the partitioning of the porosities into two components since dual porosity reservoir simulators can only handle two rock components, namely matrix system and fracture system. The goal of this study is to characterize the vugs in these systems, and to determine the pore volume compressibility for the simulation of vuggy, naturally fractured reservoirs.Sequential laboratory experiments were designed and conducted to determine the amount of secondary porosity in the core samples. A combination of capillary pressure (centrifuge and mercury injection experiments) and NMR experiments was used to determine the vug or secondary porosity of the samples from pore size and T2 (relaxation time) distributions. The results were compared and reconciled with those from porosity logs and image logs. Pore volume compressibility tests and compaction tests were used to determine the compressibility of each sample. The compaction and pore volume compressibility tests were evaluated at different net stresses to determine the influence of vuggy porosity in the samples.The composite (sample) compressibility versus porosity plots showed that pore volume compressibility increases as secondary porosity increases. This dependence, which is strong at low net stresses, gradually disappears as the reservoir pressure decreases or the net stress increases. This impliesthat the effects of secondary porosity on pore volume compressibility of the total system are minimal at low reservoir pressures. Based on these results, pore volume compressibility was generated for various values of effective and secondary porosity and served as input data to the numerical flow models. The development of the vug porosity, pore volume compressibility and the construction of the simulation flow model are described in this paper.
机译:天然裂缝型碳酸盐岩储层中通常存在三种孔隙度类型,即基质,孔隙和裂缝。在数值模拟中,通常认为孔洞连接到基体或裂缝。对这些储层进行建模的挑战之一是将孔隙分成两个部分,因为双重孔隙储层模拟器只能处理两个岩石部分,即基质系统和裂缝系统。这项研究的目的是表征这些系统中的孔洞,并确定孔洞的可压缩性,以模拟孔洞,天然裂缝性储层。 设计并进行了连续的实验室实验,以确定岩心样品中的次级孔隙度。结合毛细管压力(离心和汞注入实验)和NMR实验,根据孔径和T2(松弛时间)分布确定样品的孔洞或次生孔隙率。对结果进行了比较,并将其与孔隙度测井和图像测井的结果进行了核对。孔体积可压缩性测试和压实测试用于确定每个样品的可压缩性。在不同的净应力下评估压实度和孔体积可压缩性测试,以确定样品中孔洞孔隙率的影响。 复合材料(样品)的可压缩性与孔隙率关系图显示,孔隙体积的可压缩性随次生孔隙率的增加而增加。这种依赖关系在低净应力下很强,随着油藏压力降低或净应力增加而逐渐消失。这意味着 在较低的储层压力下,次生孔隙度对整个系统的孔隙体积可压缩性的影响最小。基于这些结果,生成了有效孔隙度和次要孔隙度的各种值的孔体积可压缩性,并将其用作数值流模型的输入数据。本文介绍了孔洞孔隙度,孔隙体积可压缩性的发展以及模拟流动模型的构建。

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