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Evaluating the Variability of the Archie Cementation Factor m in Heterogeneous Carbonates: A Case Study from a Lower Cretaceous Reservoir in UAE

机译:评价甲基胶质因子M在异构碳酸盐中的可变性:阿联酋较低白垩纪储层的案例研究

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Carbonate reservoirs introduce challenge in providing accurate water saturation from conventional Archie equation. One of the reasons is due to the variability of the Archie cementation factor "m" because of complex and tortuous nature of these heterogeneous carbonates. The study was performed by integrating core and log data from advance measurements to understand the root cause and range of the variability and an attempt to link sedimentology and diagenetic facies to petrophysical groups. The Study focused on a carbonate reservoir with complex pore network. The formation resistivity factor (FRF) measurements were conducted with high-resolution sampling on a selected well. Each of FRF plug has associated porosity, permeability, thin sections, MICP, NMR and high-resolution dual energy micro CT scan. The m value from FRF is then plotted along the porosity-permeability plot. The capillary pressure parameters (entry pressure, slope, inflexion points) were extracted from MICP and relationship is plotted against m. Diagenetic facies described from the thin sections is compared versus m. Principal component analyses was conducted to identify factors relating to m. The uncertainty on water saturation associated to variable parameter m was assessed using Monte Carlo analysis on multiple wells. An advanced multi-frequency dielectric logging tool was run on couple of wells to provide variable water-phase tortuosity (MN) measurement. Specific analysis was performed to extract the variable m value from the measurement over limited zones, which has been derived from core "m" measurements. Several wells located on the flank of the reservoir below water level were evaluated. Dean stark measurements were performed on a well and used to validate the saturation calculation. It is obvious that the evaluated reservoir has high degree of heterogeneity as indicated by complex pore network with multi modal pore system as shown by the thin sections, MICP and plug CT Scan.
机译:碳酸盐储层在传统的Archie方程提供准确的水饱和时引入挑战。其中一个原因是由于这些异质碳酸盐的复杂和曲折性质,因此原因是archie胶结因子“m”的变化。该研究是通过从预先测量中集成核心和日志数据来进行的,以了解可变性的根本原因和范围,并试图将沉积物和岩性相片链接到岩石物理组。该研究专注于碳酸盐储层,复杂的孔网络。形成电阻率因子(FRF)测量以精选的井上的高分辨率取样进行。 FRF插头中的每一个都具有相关的孔隙度,渗透性,薄部分,MICP,NMR和高分辨率双能量微CT扫描。然后沿孔隙率曲线图绘制来自FRF的M值。从MICP中提取毛细管压力参数(进入压力,斜率,拐点),并绘制关系。与薄部分中描述的成岩相比为m。进行主成分分析以识别与m有关的因素。使用蒙特卡罗分析对多个井进行评估与可变参数M相关的水饱和的不确定性。在井上进行高级多频介质测井工具,以提供可变的水相曲折(Mn)测量。执行具体分析以从有限区域的测量中提取可变M值,该测量来自核心“M”测量。评估位于水位低于水位的储层侧面上的几孔。 Dean Stark测量在井上进行,用于验证饱和度计算。显而易见的是,评估的储存器具有高度的异质性,如复合孔网络与多模态孔隙系统所示,如薄部分,MICP和插头CT扫描所示。

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