The steelmaking industry is one of the most difficult industrial sectors to decarbonise, with blast furnaces projected to play a dominant role in global iron production during this energy transition period. Iron ore behaviour remains largely unpredictable, given the uncertainty in the softening, deformation, and melting of iron-ore pellets in the cohesive zone, where small changes in gas permeability can significantly reduce furnace stability. Herein, we combine high-energy X-ray computed tomography, micro-chemical analysis, and moving particle hydrodynamics to link the internal transformation of reduced pellets with the mechanical collapse of a packed bed. Interrupted reduction–softening–melting experiments showed a progressive transition from a load-bearing metallic-iron shell at 1300 °C, to iron–slag coexistence and oxide enrichment in the core at 1400 °C, and finally to melting and dripping at 1550 °C. Three-dimensional tomography results quantified how the pellet-rich layer densifies and narrows, while particle simulations reproduced its displacement and collapse using a yield-stress formulation constrained by experimental data. This inverse calibration helped translate the observed deformation into a temperature-dependent shell-strength law. Our multiphysics framework converts tomographic images from static descriptors into predictive inputs for multi-scale furnace models, thereby offering a method to evaluate raw materials and operational strategies for low-carbon ironmaking.
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Natsui et al. (2026) studied this question.
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