4.6 Article

A Fast-Acting Method for Simulating Precipitation During Heat Treatment of Superalloy 718

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SPRINGER
DOI: 10.1007/s11661-020-06092-6

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  1. EPSRC [EP/M50726X/1] Funding Source: UKRI

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A fast-acting mean-field method for simulating precipitation of gamma '' and gamma ' phases in superalloy 718 aging process has been developed and validated through literature observations. The approach includes corrections for non-spherical shapes of precipitates, particularly for gamma '', and emphasizes the importance of selecting input material properties. Simulation results show good agreement with experimental measurements in terms of precipitate volume fraction and average size evolution, with the sensitivity of model predictions to input parameters quantified.
A fast-acting, mean-field method for simulating precipitation of the gamma '' and gamma ' phases during aging of superalloy 718 following super-delta-solvus solution treatment was formulated and validated using observations in the literature. The approach assumed classical (homogeneous) nucleation and diffusion-controlled growth (N&G) of disk/ellipsoidal-shaped-gamma '' and spherical-gamma ' particles. For the gamma '' precipitates in particular, the evolution equations for both nucleation and growth incorporated corrections for the non-spherical shape, assuming a fixed aspect ratio. In addition, special attention was paid to the choice of input material properties for simulations. These parameters included the bulk free energies of transformation, particle-matrix (misfit) elastic strain energy (for gamma ''), effective diffusivities, and the gamma ''-gamma and gamma '-gamma interface energies. The applicability of the diffusivities and interface energies chosen for the N&G simulations was established by their consistency in replicating previously measured rate constants for the diffusion-controlled coarsening of both gamma '' and gamma '. The N&G formulation was discretized to obtain numerical (spreadsheet) solutions via the Kampmann-Wagner approach. Simulation results for the temporal evolution of volume fraction and average size of the precipitates showed good agreement with experimental measurements. The sensitivity of model predictions to various input parameters was also quantified.

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