In-situ XCT DVC analysis
We investigate how internal microcracking and local deformation govern the macroscopic failure and hysteresis of crystalline rock. In-situ X-ray computed tomography (XCT), quantitative void segmentation and digital volume correlation (DVC) connect evolving three-dimensional crack networks with internal strain fields. Through uniaxial compression of fine granite, we have revealed the nucleation of isolated microcracks followed by unstable coalescence, with damage evolving from predominantly inclined cracking towards a stronger contribution from load-parallel cracks near failure [paper]. Moreover, a complete cycle of Loading–unloading–reloading observations link the mechanical hysteresis to delayed strain release in dilation zones associated with shear cracking, and reveal additional damage before the previous peak load is regained [paper]. These observations underpin micromechanical models of damage accumulation and rock fatigue.














