新奥尔巴尼页岩的多尺度孔隙表征:来自互补分析技术的见解

IF 5.2 3区 工程技术 Q2 ENERGY & FUELS
Khawaja Hasnain Iltaf, Qinhong Hu*, Majie Fan, Prince Oware, Qiming Wang, Chen Zhao, Tao Zhang, Rizwan Sarwar Awan, Danish Khan and Ali Raza, 
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引用次数: 0

摘要

从页岩地层中提取碳氢化合物变得越来越重要,需要更深入地了解其形态和结构特征,特别是孔隙类型和孔隙结构参数,这对于确定页岩油藏的储存和生产潜力至关重要。本研究通过调查伊利诺斯盆地新奥尔巴尼页岩(NAS)三种岩相孔隙的分布、形成和矿物学关系,解决了这一需求。利用扫描电镜(SEM)、氮气(N2)物理吸附、小角x射线散射(SAXS)、x射线衍射(XRD)、偏光显微镜和TOC分析,综合分析了这些岩相的孔隙结构和形态。brunauer - emmet - teller (BET)比表面积(SSA)范围为0.3 ~ 24.6 m2/g(平均5.5 m2/g),总孔容(TPV)范围为0.002 ~ 0.040 cm3/g(平均0.012 cm3/g)。结果表明,NAS具有非均质孔隙结构,孔径大小和形状各异,从NAS-1和NAS-2岩相的墨水瓶状到NAS-3岩相的楔形为主。无机孔隙,包括中孔和大孔,在孔隙系统中起着重要作用,其存在受NAS内特定岩相类型的影响。有机质孔隙在各岩相中发育有限,这可能是由于热成熟度较低所致。有机质和脆性矿物伴生的微裂缝发育较好。NAS-2岩相具有良好的孔隙结构参数,对流体运移尤为重要。深入了解不同矿物和岩相孔隙形成机制及其结构属性,对推进页岩油气勘探开发具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multiscale Pore Characterization of the New Albany Shale: Insights from Complementary Analytical Techniques

The extraction of hydrocarbons from shale formations has become increasingly important, necessitating a deeper understanding of their morphological and structural characteristics, particularly pore types and pore structure parameters, which are essential for determining the storage and productive potential of shale oil reservoirs. This research addresses this need by investigating the distribution, formation, and mineralogical relationships of pores in the three lithofacies of the New Albany Shale (NAS) in the Illinois Basin. Utilizing scanning electron microscopy (SEM), nitrogen (N2) physisorption, small-angle X-ray scattering (SAXS), X-ray diffraction (XRD), polarizing microscopy, and TOC analyses, the study comprehensively analyzes the pore structure and morphology across these lithofacies. The Brunauer–Emmett–Teller (BET) specific surface area (SSA) ranges from 0.3 to 24.6 m2/g (average of 5.5 m2/g), with the total pore volume (TPV) ranging from 0.002 to 0.040 cm3/g (average 0.012 cm3/g). The results reveal that NAS exhibits a heterogeneous pore structure, characterized by various pore sizes and shapes, varying from ink-bottle-shaped in lithofacies NAS-1 and NAS-2 to predominantly wedge-shaped in lithofacies NAS-3. Inorganic pores, including mesopores and macropores, play a significant role in the pore system, and their presence is influenced by the specific lithofacies types within NAS. Organic matter (OM) pores exhibit limited development across all lithofacies, which could be attributed to the lower thermal maturity. In contrast, microfractures associated with organic matter and brittle minerals are comparatively well-developed. The NAS-2 lithofacies is particularly important for fluid migration due to its favorable pore structure parameters. A detailed understanding of the mechanisms of pore formation and their structural attributes across different minerals and lithofacies is crucial for advancing the exploration and development of shale oil and gas deposits.

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来源期刊
Energy & Fuels
Energy & Fuels 工程技术-工程:化工
CiteScore
9.20
自引率
13.20%
发文量
1101
审稿时长
2.1 months
期刊介绍: Energy & Fuels publishes reports of research in the technical area defined by the intersection of the disciplines of chemistry and chemical engineering and the application domain of non-nuclear energy and fuels. This includes research directed at the formation of, exploration for, and production of fossil fuels and biomass; the properties and structure or molecular composition of both raw fuels and refined products; the chemistry involved in the processing and utilization of fuels; fuel cells and their applications; and the analytical and instrumental techniques used in investigations of the foregoing areas.
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