A Probabilistic Method to Populate Petrophysical Groups on Routine Core Analysis Data from Mercury Injection Capillary Pressure Domain

R. Celma, A. Lavenu
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Abstract

Analyzing capillary pressure (Pc) is one of the most common methods to create petrophysical groups in carbonates, since the Pc explains the moment when the fluid starts moving in the porous media, how easy or hard is the displacement of the fluid and when there is no further displacement (irreducible saturation of the porous media). In comparison to routine core analysis (RCA) data, MICP dataset is rather small. However, utilizing all the spectrum of data is critical, more specifically in highly heterogeneous carbonates, hence the need to populate petrophysical groups from MICP to RCA space. To determine the petrophysical groups from the MICP the following parameters were used: entry pressure, normalized porosity, permeability, rock quality index, and the hyperbolic tangent of each to the MICP samples. The petrophysical groups generated by this method give a very discrete clustering where the ranges of porosity and permeability are well defined. For distributing petrophysical groups from the MICP domain into the RCA domain, a Bayesian Inference approach in the porosity permeability space was used. Porosity and permeability standard deviation and mean for each of the petrophysical groups, were used to build a probability density functions (PDF) which will be taken as our probable scenario to feed the Bayesian Algorithm. The results from 350 MICP samples show that we could establish a reliable petrophysical groups distribution over 7000 RCA samples. In a second stage, petrophysical groups populated in the RCA space were used to train our logs and create a continuous curve of petrophysical groups that will support the property distribution in our 3D model.
用压汞毛细管压力域常规岩心分析数据填充岩石物理类群的概率方法
分析毛细压力(Pc)是在碳酸盐岩中创建岩石物理组的最常用方法之一,因为Pc可以解释流体在多孔介质中开始移动的时刻,流体位移的难易程度以及何时没有进一步的位移(多孔介质的不可还原饱和度)。与常规的核心分析(RCA)数据相比,MICP数据集相当小。然而,利用所有频谱数据至关重要,特别是在高度非均质碳酸盐中,因此需要填充从MICP到RCA空间的岩石物理组。为了从MICP中确定岩石物理组,使用了以下参数:进入压力、归一化孔隙度、渗透率、岩石质量指数以及它们与MICP样品的双曲切线。通过这种方法生成的岩石物理组给出了一个非常离散的簇,其中孔隙度和渗透率的范围是明确的。为了将岩石物理群从MICP域分布到RCA域,采用了孔隙度渗透率空间的贝叶斯推理方法。每个岩石物理组的孔隙度和渗透率的标准差和平均值被用来构建概率密度函数(PDF),该函数将作为我们的可能场景来提供贝叶斯算法。350个MICP样品的结果表明,我们可以在7000个RCA样品上建立可靠的岩石物性组分布。在第二阶段,在RCA空间中填充岩石物理组,用于训练测井曲线,并创建岩石物理组的连续曲线,以支持3D模型中的属性分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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