Microscopic pore throat structures and water flooding in heterogeneous low-permeability sandstone reservoirs: A case study of the Jurassic Yan'an Formation in the Huanjiang area, Ordos Basin, Northern China

https://doi.org/10.1016/j.jseaes.2021.104903Get rights and content

Highlights

  • The pore throat structure is classified based on inflection points of fractal curves.

  • The heterogeneity is caused by the varying proportions of micro-structure types.

  • The water flooding is mainly affected by the heterogeneity of pore throat structure.

Abstract

The complexity of the pore throat structures of heterogeneous low-permeability reservoirs causes uneven water flooding, resulting in the retention of a considerable amount of residual oil. Therefore, it is necessary to characterize pore throat structures and the effects of these structures on water flooding. Such structures and effects were investigated using scanning electron microscopy (SEM), cast thin sections (CTS), high-pressure mercury intrusion (HPMI) and microvisualization seepage experimentations. In the fractal dimension curves, there were two relatively close inflection points, corresponding to pore throat radii of approximately 3 µm and 0.02 µm. On this basis, the pore throat structures of all the samples were categorized into macrothroats, mesothroats and microthroats. All the samples contained these three types of pore throat structures. The heterogeneity of the pore throat structure was caused by the varying proportions of the different pore throat structure types. This was the first analysis of the effects of these varying proportions of pore throat structure types in one sample on water flooding. The influences of the proportions and pore throat radii of the different pore throat structures on water flooding were notable. Through this study, the effects of the pore throat structures on water flooding were found to be controlled by the proportions of the different pore throat structure types. This finding is of great significance to the efficient development of heterogeneous low-permeability reservoirs.

Introduction

Low-permeability sandstone reservoirs are important oil-producing reservoirs in the continental sedimentary basins of China. The permeability of these reservoirs is generally lower than 50 × 10−3 μm2 (Li, 2016). Their main characteristics are small pore throats, high capillary pressures and complex pore throat structures (Zeng and Li, 1994). Influenced by various geological factors, such as sedimentation and diagenesis, low-permeability reservoirs have complex pore throat structures with notable microheterogeneity (Chen et al., 2019, Li et al., 2017a, Li et al., 2017b, Liu et al., 2018, Wang et al., 2017, Wang et al., 2020). The pore throat structure greatly affects the petrophysical and oil-bearing properties of a reservoir (Cui et al., 2019, Dou et al., 2018, Qiao et al., 2019, Wang et al., 2018, Zhou et al., 2016). The shape and connectivity of pores notably impact the porosity and permeability (Desbois et al., 2011). Understanding the pore throat structure is important in reservoir evaluation and efficient development (Schmitt et al., 2015, Xiao et al., 2016). At present, the low-permeability reservoirs in China are mostly developed by water flooding to supplement formation energy (LI et al., 2015, Li, 2016). During the process of water flooding, the pore throat structure exerts an important impact on the sweep efficiency of the injected water. Li et al. (2018) analyzed the effect of pore throat structure on water flooding and found that pore throats were the most important feature affecting water flooding. The larger the pore throats are, the better the water flooding effect. Microheterogeneity imposes a major effect on water flooding. The more homogeneous a reservoir is, the lower the remaining oil saturation (LI et al., 2018a, Li et al., 2018b, Sun et al., 2013), but quantitative evidence of this relationship is lacking.

The low-permeability sandstone reservoirs of the Jurassic Yan'an Formation are important exploration and development targets in the Ordos Basin, China (Shi et al., 2011). At present, related research on pore throat characteristics has focused on mainly the tight sandstone reservoirs of the Triassic Yanchang Formation, and research on low-permeability sandstone reservoirs of the Jurassic Yan'an Formation is limited.

Considering the current insufficient research on the pore throat structures of Jurassic low-permeability reservoirs in the Ordos Basin and the limited quantitative evidence regarding the effect of pore throat structure heterogeneity on water flooding, this study was conducted. A series of laboratory investigations, such as scanning electron microscopy (SEM), cast thin sections (CTS) and high-pressure mercury intrusion (HPMI) and microvisualization seepage experimentation, was carried out on low-permeability sandstone samples collected from the Jurassic Yan'an Formation of the Ordos Basin to analyze the pore throat structures and their influence on water flooding. The effects of the microscopic pore throat structure, especially heterogeneity, on water flooding were studied. This work is of great significance for further developing heterogeneous low-permeability sandstone reservoirs.

Section snippets

Geological background

The Ordos Basin is one of several petroliferous basins located in Northern China (Fig. 1a). The Huanjiang area is located in the central part of the Tianhuan Depression of the western Ordos Basin (Fig. 1b). The Jurassic Yan'an Formation reservoirs are typical low-permeability sandstone reservoirs, and the lower section of the Yan'an Formation is the main oil-bearing layer in the study area. The lithology of the reservoir is mainly characterized as fine sandstone and siltstone (Fig. 1c).

Experimental samples

In this study, samples were collected from 6 wells of the Jurassic Yan'an Formation reservoir in the Huanjiang area of the Ordos Basin. The samples were processed into thin sections and cylinders. The helium porosity and nitrogen permeability were measured. SEM (12 samples), CTS (12 samples), HPMI (8 samples) and microvisualization seepage (6 samples) analyses were performed.

Scanning electron microscopy (SEM)

Rock characteristics such as the interstitial material, pore throat structure and cementation type can be directly

Porosity and permeability

The helium porosity of the Jurassic Yan'an Formation reservoirs in the Huanjiang area of the Ordos Basin ranges from 8.01% to 17.42%, mainly measuring between 12% and 16%, with an average porosity of 14.41%. The nitrogen permeability ranges from 1.03 to 143.62 × 10−3 μm2, with most values less than 50 × 10−3 μm2 and an average permeability of 35.08 × 10−3 μm2, which indicates low-permeability reservoirs (Li, 2016). Compared to the other reservoirs of the Ordos Basin, the Jurassic Yan'an

The heterogeneity of the pore throat structure

Pore throat structure heterogeneity is mainly reflected in two aspects: heterogeneity among samples and heterogeneity within a sample.

Conclusions

  • (1)

    The pore throat structures of the low-permeability reservoirs of the Jurassic Yan'an Formation in the Huanjiang area of the Ordos Basin exhibit high heterogeneities. Based on their fractal characteristics, the pore throat structures of the reservoir samples are categorized into three types: macrothroats, mesothroats and microthroats.

  • (2)

    The fundamental cause for the heterogeneity of the pore throat structure is the varying proportions of the three types of pore throat structures.

  • (3)

    Pore throat

CRediT authorship contribution statement

Xinyu Zhong: Methodology, Formal analysis, Writing - original draft. Yushuang Zhu: Methodology, Writing - review & editing. Tao Jiao: Data curation. Zhao Qi: Data curation. Jianghua Luo: Investigation, Data curation, Formal analysis. Yuhang Xie: Writing - review & editing. Linyu Liu: Writing - review & editing.

Declaration of Competing Interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Acknowledgments

This study was funded by the National Major Science and Technology Projects of China (2016ZX05046). This work was supported by the State Key Laboratory of Continental Dynamics and PetroChina Changqing Oilfield Company.

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