The Flow Zone Indicator (FZI) and Pore Geometry Structure (PGS) Rock Typing Comparison to Maximize Permeability Estimation on Carbonate Reservoir, Case Study: Kais Formation, Bintuni Basin

F. R. Ramadhan
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Abstract

Carbonate rock has high level of heterogeneity and it makes up the majority of reservoirs in the world, for example the Kais Formation reservoir. The heterogeneities of carbonate rock are influenced by mineral composition, diagenesis, and depositional environment. Those heterogeneities affect the permeability of the rock, so that it will produce a very high uncertainty in the formation evaluation process. The permeability value is one of the vital parameters in a reservoir, so it must be predicted with a high degree of accuracy. One of the ways is to characterize the reservoir using rock typing. Rock typing is performed in conventional coring data at1553 – 1738 feet MD), with 55 RCAL samples and capillary pressure (Pc). Rock typing begins by considering the geological features of the rock composition (lithology, colour, texture, mineral composition, diagenesis and depositional facies). Then the rock type Flow Zone Indicator (FZI) is obtained based on the calculation of the Rock Quality Index (RQI) and the normalization of the porosity value (ϕz), as well as rock type PGS which is used a comparison between pore structure and pore geometry. From those core analysis, there are with 6 rock types FZI, and with10 rock types PGS. The comparison of the predicted permeability values was carried out based on the equations from the rock typing results in each method. The permeability predictions using the FZI method showed a better level of relevance to the permeability values of the core data. In the un-cored well interval, cluster analysis was performed for rock typing which resulted in an undetailed rock type log as a calibration log for the Self Organizing Map (SOM) algorithm analysis, which produced a detailed rock type log, before re-doing the FZI analysis. The results of the estimated permeability (K) of FZI in the un-cored well intervals have correlation coefficient between 0.76 – 0.86 to the synthetic permeability log in the majority of available wells. New Rock Type (RT) for each well shows that RT-4 and RT-5 have fairly high value of flow units which indicates as good rock types in flowing fluids.
流动带指标(FZI)与孔隙几何结构(PGS)岩石类型对比研究——以宾图尼盆地凯伊斯组为例
碳酸盐岩具有高度的非均质性,在世界储层中占绝大多数,如凯斯组储层。碳酸盐岩的非均质性受矿物组成、成岩作用和沉积环境的影响。这些非均质性影响了岩石的渗透率,因此在储层评价过程中会产生很大的不确定性。渗透率是储层的重要参数之一,因此对渗透率的预测必须达到较高的精度。其中一种方法是利用岩石类型来描述储层。岩石类型是在1553 - 1738英尺深度的常规取心数据中进行的,使用了55个RCAL样品和毛细管压力(Pc)。岩石分型首先考虑岩石组成的地质特征(岩性、颜色、质地、矿物组成、成岩作用和沉积相)。然后通过岩石质量指数(RQI)的计算和孔隙度值(ϕz)的归一化,得到岩石型流区指标(FZI),以及岩石型PGS(孔隙结构和孔隙几何形状的比较)。通过岩心分析,发现FZI有6种岩石类型,PGS有10种岩石类型。根据各方法岩石分型结果的方程,对预测渗透率值进行了比较。利用FZI方法预测的渗透率与岩心数据的渗透率值具有更好的相关性。在未取心井段,在重新进行FZI分析之前,对岩石类型进行了聚类分析,得到了一份不详细的岩石类型日志,作为自组织图(SOM)算法分析的校准日志,生成了一份详细的岩石类型日志。FZI在未取心井段的渗透率(K)估计值与大多数可用井的综合渗透率测井值的相关系数在0.76 ~ 0.86之间。每口井的新岩石类型(RT)表明,RT-4和RT-5具有较高的流动单位值,表明它们是流动流体中较好的岩石类型。
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