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The regularisation length (\ell) controls the width of the diffusive crack zone ((\approx 3\ell)). When (\ell\to0), (\Pi) (\Gamma)-converges to the classical Griffith functional. Stationarity of (\Pi) with respect to admissible variations (\delta\mathbfu) and (\delta\phi) yields the coupled Euler‑Lagrange equations :
[ \eta_e = \int_\Omega_e \ell |\nabla\phi^h|^2 ,\mathrmdV . \tag6 ] Working Model 2d Crack-
Corresponding author : first.author@univa.edu A robust computational framework for simulating quasi‑static fracture in brittle solids is presented. The model couples linear elasticity with a regularized phase‑field description of cracks, yielding a fully variational formulation that naturally captures crack nucleation, branching, and interaction without explicit tracking of the crack surface. The governing equations are derived from the minimisation of the total free energy, leading to a coupled system of a displacement‑balance equation and a diffusion‑type phase‑field evolution equation. An adaptive finite‑element discretisation with a staggered solution scheme is implemented in 2‑D. Benchmark problems—including the single‑edge notched tension test, the double‑cantilever beam, and a complex multi‑crack interaction case—demonstrate excellent agreement with analytical solutions and experimental data. Sensitivity analyses reveal the influence of the regularisation length, fracture energy, and load‑control strategies on crack paths. The presented workflow constitutes a “working model” that can be readily extended to anisotropic, heterogeneous, or dynamic fracture problems. The regularisation length (\ell) controls the width of
[ G = \frac{P^2
The first equation is the for a degraded material. The second is a reaction‑diffusion equation governing the evolution of the crack field. Irreversibility is enforced by a history field (H(\mathbfx) = \max_t\le t\psi^+(\boldsymbol\varepsilon(\mathbfx,t))) so that the tensile energy term never decreases: \tag6 ] Corresponding author : first