Complete understanding of any natural phenomenon can only be achieved by explicitly expressing it in terms of primitive variables. The laws of thermodynamics have been extensively studied for centuries, accelerating societal progress through developments across several branches of science and technology. Phase nucleation can be observed in the melting and freezing of rocks and ice caps, abundant shapes of snow flocks, rain regimes, snowfall, casting, and metal forming, among other applications. The most challenging aspect of nucleation is the equilibrium shift controlled by the gradients in temperatures, species, work, and other variables, in accordance with the first law of thermodynamics, which defines the thermal field. In this study, the thermal field and thermal field tensor were defined in terms of equilibrium dislocations to assess their primitive variables. Theoretical simulations for the Gibbs–Thomson coefficients were applied to predict the experimental microstructure evolution.
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