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Fractal analysis of tight gas sandstones using high-pressure mercury intrusion techniques

机译:利用高压汞压入技术对致密气砂岩的分形分析

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Pore structure is one of important factors affecting the properties of sedimentary rocks, however, it is difficult to describe microscopic parameters of the pore structure such as pore geometry, pore-size distribution, and pore space topology. Fractal theory is an effective and available method to quantify the complex and irregular pore structure of rocks. Routine rock properties measurements and high-pressure mercury intrusion tests (HPMI) were performed on a suite of the Bashijiqike tight gas sandstone samples to delineate the pore network characteristics of these reservoir rocks. Thin section epifluorescence and scanning electron microscopy (SEM) analyses were used to gain insight into pore geometry and pore size distribution of these sandstones.
机译:孔隙结构是影响沉积岩特性的重要因素之一,但是,很难描述孔隙结构的微观参数,例如孔隙几何形状,孔径分布和孔隙空间拓扑。分形理论是量化岩石复杂和不规则孔隙结构的有效方法。在一组Bashijiqike致密气砂岩样品上进行了常规岩石性能测量和高压汞侵入测试(HPMI),以描绘出这些储集层岩石的孔隙网络特征。薄截面落射荧光和扫描电子显微镜(SEM)分析用于深入了解这些砂岩的孔隙几何形状和孔径分布。

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