Petrophysical Charaterizations of Some Reservoir Formations in Ghani Oilfield, Libya

Ibrahim Abou El Leil
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Abstract

This study has been conducted on three types of reservoir rocks for core analysis of samples denoted by R-1, R-2 and R-3 of Ghani oil field from three reservoir include Farrud, Facha and Mabruk formations respectively. This analysis includes determination of physical characteristics e. g. porosity ( ), permeability (k), formation factor (FF) and resistivity index (RI). The purpose of this study is to how core petrophysical data might be most investigating effectively applied to the petrophysical prediction of petrophysical properties from core samples analysis. For Farrud reservoir of R-1 shows that the relation between degree of saturation ( ) and relative oil permeability(Kro) equal the relative permeability of water(Krw) at which the intersection point between the two curves ; whereas, the flow with the same rate. FF and RI are vary with and the RI is a function of . The gas-oil relative permeability have been expressed graphically. Whereas, the intersection point between the two curves (Kro) equal the (Krg), at which both oil and gas are flow with the same rate. A similar results were obtained from Facha reservoir, R-2. The petrophysical properties of core samples for R-3 of Mabruk Formation have been performed including , k, and . The comparison between the three reservoirs by correlation between the average values such as , k, grain density and RI; shows that the average of Mabruk reservoir k greater than the other two reservoirs, while the other properties seem to be close together.
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利比亚加尼油田部分储层岩石物理特征
本研究对三种类型的储层岩石进行了岩心分析,样品分别为R-1、R-2和R-3,分别来自Farrud、Facha和Mabruk三个储层。该分析包括确定物理特征,如孔隙度()、渗透率(k)、地层因子(FF)和电阻率指数(RI)。本研究的目的是研究岩心岩石物性数据如何最有效地应用于岩心样品岩石物性分析的岩石物性预测。对于R-1 Farrud油藏,饱和度()与相对油渗透率(Kro)的关系等于两者曲线交点处的相对水渗透率(Krw);然而,以相同的速率流动。FF和RI随的变化,而RI是的函数。用图形表示了气-油相对渗透率。而两条曲线的交点(Kro)等于(Krg),在该点处油气以相同的速率流动。在R-2的Facha储层也得到了类似的结果。测量了Mabruk组R-3岩心样品的岩石物理性质,包括、k和。利用k、颗粒密度、RI等平均值的相关性对3个储层进行对比;结果表明,马布鲁克储层的平均k值大于其他两个储层,而其他储层的性质基本接近。
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