4.7 Article

Rock grain-scale mechanical properties influencing hydraulic fracturing using Hydro-GBM approach

期刊

ENGINEERING FRACTURE MECHANICS
卷 262, 期 -, 页码 -

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.engfracmech.2021.108227

关键词

Distinct element method; Hydro-GBM; Micro mechanism; Calibration; Hydraulic fracturing; Particle Flow Code

资金

  1. China Scholarship Council (CSC) -Monash University Postgraduate Scholarship [CSC201708150112]
  2. Monash University Faculty of Engineering Graduate Research International Exchange Award

向作者/读者索取更多资源

Rock cracking and fracturing have significant implications for geological applications. This study investigates the influence of rock grain-scale mechanical parameters on fluid-driven cracking behaviors and proposes a formulation to eliminate the mismatch between experimental and simulated shear cracking. The results provide valuable insights into the effects of rock grain-scale properties on hydraulic fractures and guide the selection and calibration of micro mechanical parameters in future modeling.
Rock cracking is of key concern to many geological applications. On a grain scale, rock fracturing depends on not only the external load but also the mechanical properties of the mineral grain and grain boundary. In this study, we investigated the effect of rock grain-scale mechanical param-eters on fluid-driven cracking behaviours and discussed the identification of micro mechanical parameters in the grain-based model. A coupled hydro-grain-based DEM model (Hydro-GBM) is used to reconstruct rock microstructures and simulate hydraulic fracturing. We analyzed the influences of the main micro-mechanical parameters of mineral grain and grain boundary and explored the responsible micro-mechanisms. Results including crack initiation pressure, break-down pressure, partitions of intragranular and grain boundary cracks in tension/shear are pre-sented in detail. Then, based on the parameter analysis, some issues in identifying micro parameters in existing DEM simulations are discussed. We proposed a formulation to determine contact friction angle, which could eliminate the long-standing mismatch of shear cracking be-tween experiment and simulation. We also suggested the importance of calibrating micro results in grain-based modelling. The presented study systematically revealed the effects of rock grain-scale properties on hydraulic fractures and could provide valuable references to the selection of micro mechanical parameters in future modelling.

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