利用纳米ct技术定量表征致密砂岩储层渗透率非均质性——以鄂尔多斯盆地延长组为例

IF 3.6
Junlong liu , Xiangchun Zhang
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引用次数: 0

摘要

储层物性是影响储层渗流能力的重要因素。由于微纳米级孔喉系统的广泛发展,致密砂岩储层表现出复杂的孔喉连通性。利用无损定量方法表征致密砂岩储层微观物性,是确定致密砂岩储层微观孔喉特征及其影响储层孔隙度和渗透率机理的重要手段。本研究采用高分辨率纳米CT技术对鄂尔多斯盆地低渗透砂岩样品和两种致密砂岩样品进行无损检测,定量表征其微观孔喉结构,并基于CT阈值差异和灰度模型对其进行三维建模。分析对比表明,三种样品的孔隙度和渗透率均表现出一定的正相关关系,但影响孔隙度和渗透率的最重要因素是微观孔喉结构。孔隙数量对致密砂岩孔隙度的影响较小,但大于20 μm的大孔隙对孔隙度的影响较大,表明致密砂岩的渗透率主要受大孔喉的控制。对于这些样品,较高的渗透率对应于较大的平均喉道尺寸。因此,平均半径大于2 μm的喉道可以显著提高致密砂岩的渗透率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Quantitative characterization of permeability heterogeneity of tight-sand reservoirs using nano-CT technology: A case study of the Yanchang Formation, Ordos Basin

Quantitative characterization of permeability heterogeneity of tight-sand reservoirs using nano-CT technology: A case study of the Yanchang Formation, Ordos Basin
The physical properties of hydrocarbon reservoirs are important factors affecting the percolation ability of the reservoirs. Tight-sand reservoirs exhibit complex pore throat connectivity due to the extensive development of micro- and nano-scale pore and throat systems. Characterizing the microscopic properties of these reservoirs using nondestructive, quantitative methods serves as an important means to determine the characteristics of microscopic pores and throats in tight-sand reservoirs and the mechanism behind the influence of these characteristics on reservoir porosity and permeability. In this study, a low-permeability sandstone sample and two tight sandstone samples collected from the Ordos Basin were nondestructively tested using high-resolution nano-CT technology to quantitively characterize their microscopic pore throat structures and model them three-dimensionally (in 3D) based on CT threshold differences and gray models. A thorough analysis and comparison reveal that the three samples exhibit a certain positive correlation between their porosity and permeability but the most important factor affecting both porosity and permeability is the microscopic pore throat structure. Although the number of pores in tight sandstones shows a minor impact on their porosity, large pores (more than 20 μm) contribute predominantly to porosity, suggesting that the permeability of tight sandstones is controlled primarily by large pore throats. For these samples, higher permeability corresponds to larger average throat sizes. Therefore, throats with average radii greater than 2 μm can significantly improve the permeability of tight sandstones.
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