4.7 Article

Implementation of an Empirical Joint Constitutive Model into Finite-Discrete Element Analysis of the Geomechanical Behaviour of Fractured Rocks

期刊

ROCK MECHANICS AND ROCK ENGINEERING
卷 49, 期 12, 页码 4799-4816

出版社

SPRINGER WIEN
DOI: 10.1007/s00603-016-1064-3

关键词

Finite-discrete element method; Joint constitutive model; Fractures; Roughness; In situ stress

资金

  1. itf-ISF project 'Improved Simulation of Faulted and Fractured Reservoirs'
  2. Department of Earth Science and Engineering, Imperial College London
  3. EPSRC [EP/H030123/1] Funding Source: UKRI
  4. NERC [NE/L000660/1] Funding Source: UKRI

向作者/读者索取更多资源

An empirical joint constitutive model (JCM) that captures the rough wall interaction behaviour of individual fractures associated with roughness characteristics observed in laboratory experiments is combined with the solid mechanical model of the finite-discrete element method (FEMDEM). The combined JCM-FEMDEM formulation gives realistic fracture behaviour with respect to shear strength, normal closure, and shear dilatancy and includes the recognition of fracture length influence as seen in experiments. The validity of the numerical model is demonstrated by a comparison with the experimentally established empirical solutions. A 2D plane strain geomechanical simulation is conducted using an outcrop-based naturally fractured rock model with far-field stresses loaded in two consecutive phases, i.e. take-up of isotropic stresses and imposition of two deviatoric stress conditions. The modelled behaviour of natural fractures in response to various stress conditions illustrates a range of realistic behaviour including closure, opening, shearing, dilatancy, and new crack propagation. With the increase in stress ratio, significant deformation enhancement occurs in the vicinity of fracture tips, intersections, and bends, where large apertures can be generated. The JCM-FEMDEM model is also compared with conventional approaches that neglect the scale dependency of joint properties or the roughness-induced additional frictional resistance. The results of this paper have important implications for understanding the geomechanical behaviour of fractured rocks in various engineering activities.

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