Application of PCA in the Porosity Evaluation of a Coal Reservoir

Jingang Wu, Guang Zhang
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Abstract

In this paper, we study the feasibility of applying the principal component analysis (PCA) for porosity evaluation of a coal Reservoir. The geological characteristics of the No. 3 coal reservoir in Qinshui Basin (Shanxi Province, China) were analyzed at first. On this basis, vitrinite reflectance, coal macrolithotype, ash content, macro-fissure density, micro-fissure density, and coal structure were adopted as the index variables for evaluating the porosity. Three principal components were extracted by reducing dimensions of the six primitive variables. Then, a scoring model of the principal components was constructed to calculate the comprehensive scores for porosity of the coal samples. In addition, Qinshui Basin was partitioned into four regions: a (Yangquan), b (Jingfang-Wangzhuang), c (Changcun), and d (Jincheng), which were listed in a descending order as a, c, b, and d with reducing porosities. Explanation of the principal components and geological theoretical analysis revealed that the geotectonic movements and evolutions, and sedimentary environment are main controlling factors for studying the porosity based zoning of the research region. The results prove that it is feasible to apply PCA to evaluate the porosity of coal reservoirs.
主成分分析法在煤储层孔隙度评价中的应用
本文研究了主成分分析(PCA)在煤储层孔隙度评价中的可行性。首先分析了沁水盆地3号煤储层的地质特征。在此基础上,以镜质体反射率、煤的宏观岩型、灰分、宏观裂隙密度、微观裂隙密度和煤的结构作为评价孔隙度的指标变量。通过对6个原始变量降维提取3个主成分。然后,构建主成分评分模型,计算煤样孔隙度综合评分。将沁水盆地划分为a区(阳泉)、b区(京坊—王庄)、c区(长村)、d区(晋城)4个区域,按孔隙度递减顺序依次为a、c、b、d。主成分解释和地质理论分析表明,大地构造运动演化和沉积环境是研究研究区孔隙分带的主要控制因素。结果表明,用主成分分析法评价煤储层孔隙度是可行的。
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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