A micromechanics-based variational phase-field model for fracture in geomaterials with brittle-tensile and compressive-ductile behavior
Jacinto Ulloa, Jef Wambacq, Roberto Alessi, Esteban Samaniego, Geert, Degrande, Stijn Fran\c{c}ois

TL;DR
This paper introduces a micromechanics-based variational phase-field model for geomaterials that captures brittle and ductile fracture behaviors under various loading conditions, emphasizing microcrack mechanisms and non-associative frictional sliding.
Contribution
The model uniquely links microcrack evolution to damage and plasticity, providing a physically grounded approach to simulate complex fracture modes without heuristic modifications.
Findings
Accurately models tensile, shear, and mixed-mode fractures.
Captures brittle-to-ductile transition in geomaterials.
Demonstrates realistic failure modes aligned with experiments.
Abstract
This paper presents a framework for modeling failure in quasi-brittle geomaterials under different loading conditions. A micromechanics-based model is proposed in which the field variables are linked to physical mechanisms at the microcrack level: damage is related to the growth of microcracks, while plasticity is related to the frictional sliding of closed microcracks. Consequently, the hardening/softening functions and parameters entering the free energy follow from the definition of a single degradation function and the elastic material properties. The evolution of opening microcracks in tension leads to brittle behavior and mode I fracture, while the evolution of closed microcracks under frictional sliding in compression/shear leads to ductile behavior and mode II fracture. Frictional sliding is endowed with a non-associative law, a crucial aspect of the model that considers the…
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