The Hybrid Lattice/Discrete Element Method is proposed for Bonded Block Modeling of rocks. The method is a combination of the Rigid Body Spring Network Lattice Model with the Discrete Element Method. The main advantages of the new method are: (i) it operates based on either a homogeneous or heterogeneous material assumption, with heterogeneity being represented by means of the Weibull probability distribution applied to elasticity and strength parameters; and (ii) it provides for a direct material calibration scheme for rock models based on both assumptions, which does not require trial-and-error iterations. Thirteen rock types, including igneous, metamorphic, and sedimentary ones were simulated in the two-dimensional version of the method considering both assumptions, and their numerical macroscale properties were compared to the laboratory ones. Results show that while deformability and peak strength properties were accurately represented by the homogeneous models, linear elastic-brittle behavior manifested. On the other hand, the heterogeneous models presented non-linear stress–strain behavior and provided reasonable matches for the following laboratory properties: Young modulus, Poisson’s ratio, crack initiation stress, crack damage stress, unconfined compression strength, and direct tensile strength.
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