Abstract

Producing a sufficient volume of multiscale crack networks is key to enhancing recovery of shale gas. The formation of crack network largely depends on initiation and propagation of microcracks. To reveal the influence of different loading methods on the propagation of mineral-scale microcracks, this study used the Voronoi tessellation technique to establish a cohesive zone model of shale mineral distribution and applied six different boundary conditions to represent different loading methods. Crack path characteristics, rupture characteristics, continuous crack propagation and turning, and en echelon intermittent crack propagation under different loading methods were compared and analyzed. The essence of different loading methods affecting the length and complexity of cracks was the spreading range of tensile microcracks. The mechanical properties of minerals led to dissimilarities in continuous crack propagation and turning. The formation and propagation of en echelon intermittent fractures of different scales were mainly impacted by the heterogeneity of minerals and mineral aggregates. The spreading direction and connection form of en echelon intermittent fractures were mainly affected by the loading method. Conclusions arising from mineral-scale simulations contribute to understanding the mechanism of microcrack propagation resulting from different loading methods, and these conclusions have a guiding significance to enhanced shale gas recovery.

Highlights

  • Shale gas exists in low-porosity and low-permeability shale formations

  • (1) e essence of different loading methods affecting crack length and complexity was the spread range of tensile microcracks

  • Shear loading only produced parallel tensile microcracks on the right side of the maximum shear line, and the cracks tended to extend along the direction of the maximum shear force, resulting in a shorter crack length and low complexity

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Summary

Introduction

Shale gas exists in low-porosity and low-permeability shale formations. Producing a sufficient volume of multiscale crack networks is the key to enhancing the recovery of shale gas. Saadat and Taheri [26] carried out uniaxial compression experiments based on the cohesive contact model of PFC to study the formation and propagation of microcracks in the shear zone. Observations of hydraulic fracturing cracks show that the characteristics of microcracks produced by tensile, shear, tension-shear, and compression-shear are different [28,29,30]. Other experimental studies focused on tensile and threepoint bending loading, and the observed crack network and microcrack propagation were found to be quite different from uniaxial compression [9, 31]. To reveal the influence of different loading methods on the propagation of mineral-scale microcracks, this study used the Voronoi tessellation technique to establish a cohesive zone model (CZM) based on mineral distribution. E comparative analysis uncovered the mechanism of how different loading methods affect the growth of mineral-scale microcracks

Cohesive Zone Model Based on Mineral Distribution
Mathematical Model
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Findings
Discussion
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