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.
[ G = \frac{P^2
All source files are provided in the supplementary material (GitHub repository github.com/YourGroup/2DPhaseFieldCrack ). 4.1. Benchmark 1 – Single‑Edge Notched Tension (SENT) Geometry : rectangular plate (L=1.0) m, (H=0.5) m, notch length (a_0=0.2) m. Material : (E=30) GPa, (\nu=0.2), (G_c=2.7) kJ/m(^2). Parameters : (\ell = 2.5,h_\min) (where (h_\min) is the smallest element size after refinement). Working Model 2d Crack-
The load‑displacement curve obtained with the phase‑field model matches the analytical LEFM prediction for the critical stress intensity factor (K_IC= \sqrtE G_c). The computed (F_c= 4.58) kN is within 2 % of the analytical value. The crack path follows the straight line of the notch, confirming the absence of mesh bias.
[ \Delta W = \int_\Gamma_N \mathbft\cdot \Delta\mathbfu,\mathrmdS . \tag7 ] Corresponding author : first
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 :
where (N_n) is the number of nodes. Quadratic interpolation is essential to resolve the steep gradients of (\phi) within the diffusive crack zone. A goal‑oriented error estimator based on the phase‑field gradient is used: \qquad \phi^h(\mathbfx) = \sum i=1^N_n N_i(\mathbfx)
[ \mathbfu^h(\mathbfx) = \sum_i=1^N_n \mathbfN_i(\mathbfx) , \mathbfu i, \qquad \phi^h(\mathbfx) = \sum i=1^N_n N_i(\mathbfx) , \phi_i, \tag5 ]