Linxing-Shenfu Gangue Interaction Coal Seam Hydraulic Fracture Cross-Layer Expansion Mechanism

The deep coal reservoir in Linxing-Shenfu block of Ordos Basin is an important part of China’s coalbed methane resources. In the process of reservoir reconstruction, the artificial fracture morphology of coal seam with gangue interaction is significantly different, which affects the efficient development of coalbed methane resources in this area. In this paper, the surface outcrop of Linxing-Shenfu block is selected, and three kinds of interaction modes between gangue and coal seam are set up, including single-component coal rock sample, coal rock sample with different thicknesses of gangue layer and coal rock sample with different numbers of gangue. Through true triaxial physical simulation and three-dimensional discrete element numerical simulation, the law of artificial fracture initiation and propagation in multi-gangue interaction coal seam is analyzed in depth, and the hydraulic fracture initiation and propagation mode under different interaction modes of gangue layer in Linxing-Shenfu deep coal reservoir was clarified. The research shows that the initiation of artificial fractures in a single coal seam is affected by geological-engineering factors. The maximum principal stress dominates the direction of fracture propagation, and the stress difference controls the fracture morphology. When the stress difference is 2 MPa, the fracture morphology is complex, which is easy to connect to the weak surface of coal and rock cleat, and the fracture morphology of the stress difference is mainly a single main fracture. After the thickness of the gangue layer is increased from 2 to 5 cm, it is difficult for the artificial fracture to penetrate the layer vertically after the fracture initiation, and the effective transformation area of the reservoir is limited. The more the number of gangue layers, the greater the hydraulic energy consumption in the process of fracture propagation, and the more difficult the fracture propagation.

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Publication Details

Journal
Energy Engineering
Published
2025-12-25
DOI
https://doi.org/10.32604/ee.2025.068653
Primary Topic
Rock Mechanics and Modeling
Type
article
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article

Linxing-Shenfu Gangue Interaction Coal Seam Hydraulic Fracture Cross-Layer Expansion Mechanism

Xuesong Xing, Heng WEN, Jingyu Zi, Ying Zhu et al.
Energy Engineering
Rock Mechanics and Modeling
article

Linxing-Shenfu Gangue Interaction Coal Seam Hydraulic Fracture Cross-Layer Expansion Mechanism

Xuesong Xing, Heng WEN, Jingyu Zi, Ying Zhu, Qingwei Zeng, Li Wang, Yanan Hou
article en

Abstract

The deep coal reservoir in Linxing-Shenfu block of Ordos Basin is an important part of China’s coalbed methane resources. In the process of reservoir reconstruction, the artificial fracture morphology of coal seam with gangue interaction is significantly different, which affects the efficient development of coalbed methane resources in this area. In this paper, the surface outcrop of Linxing-Shenfu block is selected, and three kinds of interaction modes between gangue and coal seam are set up, including single-component coal rock sample, coal rock sample with different thicknesses of gangue layer and coal rock sample with different numbers of gangue. Through true triaxial physical simulation and three-dimensional discrete element numerical simulation, the law of artificial fracture initiation and propagation in multi-gangue interaction coal seam is analyzed in depth, and the hydraulic fracture initiation and propagation mode under different interaction modes of gangue layer in Linxing-Shenfu deep coal reservoir was clarified. The research shows that the initiation of artificial fractures in a single coal seam is affected by geological-engineering factors. The maximum principal stress dominates the direction of fracture propagation, and the stress difference controls the fracture morphology. When the stress difference is 2 MPa, the fracture morphology is complex, which is easy to connect to the weak surface of coal and rock cleat, and the fracture morphology of the stress difference is mainly a single main fracture. After the thickness of the gangue layer is increased from 2 to 5 cm, it is difficult for the artificial fracture to penetrate the layer vertically after the fracture initiation, and the effective transformation area of the reservoir is limited. The more the number of gangue layers, the greater the hydraulic energy consumption in the process of fracture propagation, and the more difficult the fracture propagation.

Energy EngineeringVol. 123(2)
Affordable and clean energy
Openalex Percentile: Top 42%
Rock Mechanics and Modeling
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Linxing-Shenfu Gangue Interaction Coal Seam Hydraulic Fracture Cross-Layer Expansion Mechanism — Xuesong Xing, Heng WEN, et al. · Energy Engineering (2025) | TGRS Research Map | TGRS