Modeling of Microsegregation and Homogenization of 6xxx Al-Alloys Including Precipitation and Strengthening During Homogenization Cooling
Abstract
:1. Introduction
2. Materials and Experimental Procedures
3. Modeling Approaches
3.1. General Description
3.2. Microsegragation During Solidification
3.3. Homogenization (Holding)
3.4. Homogenization Cooling
- The diffusion coefficients were considered constant with respect to element concentration.
- Precipitation was controlled by the diffusion of Mg, as it is the dominant component of Mg2Si.
- The dilution in the matrix was considered infinite.
- Mg2Si particles were considered spherical and with stoichiometric composition.
- There was no interaction of the diffusion fields around the particles.
- The cooling rate was slow enough, so that transient diffusion effects were minimal and thus quasi-steady state conditions could be assumed.
4. Results
4.1. Microsegregation of As-Cast Alloy
4.2. Homogenization Holding
- Si (diamond) rapidly dissolves, as it is consumed by Mg2Si that grows in the same location near the grain boundary. Simultaneously Mg2Si gradually dissolves from the grain interior to the boundary as Si and Mg migrate to the grain center. The excess Si released from the dissolution of the Si (diamond) phase, causes β-AlFeSi to grow against α-AlFeSi at the early stages of homogenization. After the complete dissolution of Si (diamond), the transformation reverses, as α-AlFeSi gradually consumes β-AlFeSi completely.
- The profiles of α-AlFeSi and β-AlFeSi exhibit an exact spatial correspondence. Where there is a drop in the fraction of β-AlFeSi, there is a rise in the fraction of α-AlFeSi and vice versa, at the same location.
- The phase fraction profiles are steeper, and the transformation is faster in the smaller grain. Yet the kinetics of β-AlFeSi→α-AlFeSi transformation in the small grain were severely hindered since α-AlFeSi was completely consumed during the early stages. A nucleation event is required to regrow α-AlFeSi, effectively reducing the rate of the transformation.
- The concentration profiles for Mg, Si and Mn become more uniform with homogenization time. The profile for Fe in FCC change mostly due to its absorption from the formation of α-AlFeSi and β-AlFeSi since the diffusivity of Fe in Al is very low.
- The average concentration of Mg and Si in the matrix interior (away from the boundary) increases with homogenization time, especially in the smaller grain.
- The profiles homogenize faster in the smaller grain due to a shorter diffusion distance.
- The compositional fluctuations close to the boundary are due to the dissolution of Mg2Si, Si (diamond) and the β-AlFeSi→α-AlFeSi transformation. These fluctuations decay with homogenization time.
- The spatial evolution of the concentration profiles is consistent with the spatial evolution of the phase fractions.
4.3. Homogenization Cooling
5. Conclusions
- A Dual-Grain Model (DGM) has been developed to describe the effect of grain size inhomogeneity during homogenization of 6082 Al alloy. The transformation of β-AlFeSi to α-AlFeSi proceeds in two steps. First, the reverse transformation takes place as β-AlFeSi grows against α-AlFeSi due to the excess Si released from the dissolution of the Si (diamond) phase. The forward transformation of β to α-AlFeSi commences once dissolution of the Si (diamond) phase is completed.
- During the transformation, the fractions of α-AlFeSi and β-AlFeSi exhibit an exact spatial and temporal correspondence. The DGM model predictions are in good agreement with experimental data.
- The KWN precipitation model was applied to the binary Al-Mg2Si system in 6005, 6063, and 6082 Al alloys. The model indicated the development of a bimodal particle size distribution during homogenization cooling, arising from corresponding nucleation events. The associated strengthening arises from contributions due to solid solution and precipitation strengthening and is in good agreement with experimental results.
- The proposed modeling approach is a valuable tool for the prediction of microstructure evolution during the homogenization of extrudable 6xxx aluminum alloys, including the often-neglected part of homogenization cooling.
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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Al-Alloy | Mg | Si | Fe | Mn |
---|---|---|---|---|
6063 | 0.5346 | 0.4194 | 0.1895 | 0.0311 |
6005 | 0.4896 | 0.686 | 0.1552 | 0.2227 |
6082 | 0.63 | 0.9 | 0.2 | 0.45 |
Process | Phenomena Modeled | Relevant Models |
---|---|---|
Casting/Solidification | Microsegregation of elements and phases | Scheil-Gulliver |
Homogenization (holding) | Dissolution of Mg2Si Transformation of β-AlFeSi to α-Al(FeMn)Si | Multicomponent, multiphase diffusion—Dual Grain Model (DGM) |
Homogenization (cooling) | Precipitation of Mg2Si Precipitation Strengthening | Kampmann-Wagner Numerical (KWN) precipitation model—Strength model |
Phase Fractions | Calculated (%) | Measured (%) |
β-AlFeSi + α-AlFeSi | 0.587 | 0.607 |
Mg2Si | 0.313 | 0.365 |
Quaternary Eutectic | 0.411 | 0.41 |
Matrix Composition Close to Boundary | Calculated (mass%) (at 0.92 Fraction of Solid) | Measured (mass%) |
Si | 1.33 | 1.2 (σ = 0.1) |
Mg | 0.6 | 0.7 (σ = 0.1) |
Mn | 0.63 | 0.3 (σ = 0.1) |
Fe | 0.003 | 0 (σ = 0.01) |
Al | 97.4 | 97.8 (σ = 0.2) |
Parameter | Symbol | Value | Source |
---|---|---|---|
Concentration of Mg in Mg2Si | (wt%) | 63.4 | Stoichiometry |
Pre-exponential term for diffusion of Mg | (m2/s) | 2.2 × 10−4 | [44] |
Activation energy for diffusion of Mg | (J/mol) | 130,000 | [44] |
Nucleus/matrix interfacial energy (Mg2Si) | (J/m2) | 0.5 | [51] |
Molar volume Mg2Si | (m3/mol) | 3.95 × 10−5 | [51] |
Total bulk nucleation site density | (#/m3) | 1019–1020 | Adjustable parameter |
Dimensionless term in activation energy for nucleation | 4 × 10−19 | [42] | |
Transition radius for precipitation strengthening | (m) | 5 × 10−9 | [52] |
Constant contribution to yield strength | (MPa) | 10 | [52] |
Parameter for solid solution strengthening of Si | 66.3 | [53] | |
Parameter for solid solution strengthening of Mg | 29 | [53] | |
Parameter for precipitation hardening | 4 × 10−6 | [42] |
Alloy | Specimen | σyield (ΜPa) | σyield Mean (MPa) | εfracture (%) |
---|---|---|---|---|
6005 | 1st | 72 | 70.33 | 27.7 |
2nd | 69 | 25 | ||
3rd | 70 | 26.3 | ||
6063 | 1st | 52 | 52.33 | 33.3 |
2nd | 53 | 30.5 | ||
3rd | 52 | 30.5 | ||
6082 | 1st | 83.75 | 88.91 | 16.6 |
2nd | 90 | 15.2 | ||
3rd | 93 | 16.6 |
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Sarafoglou, P.I.; Serafeim, A.; Fanikos, I.A.; Aristeidakis, J.S.; Haidemenopoulos, G.N. Modeling of Microsegregation and Homogenization of 6xxx Al-Alloys Including Precipitation and Strengthening During Homogenization Cooling. Materials 2019, 12, 1421. https://doi.org/10.3390/ma12091421
Sarafoglou PI, Serafeim A, Fanikos IA, Aristeidakis JS, Haidemenopoulos GN. Modeling of Microsegregation and Homogenization of 6xxx Al-Alloys Including Precipitation and Strengthening During Homogenization Cooling. Materials. 2019; 12(9):1421. https://doi.org/10.3390/ma12091421
Chicago/Turabian StyleSarafoglou, Panagiota I., Alexandros Serafeim, Ioannis A. Fanikos, John S. Aristeidakis, and Gregory N. Haidemenopoulos. 2019. "Modeling of Microsegregation and Homogenization of 6xxx Al-Alloys Including Precipitation and Strengthening During Homogenization Cooling" Materials 12, no. 9: 1421. https://doi.org/10.3390/ma12091421
APA StyleSarafoglou, P. I., Serafeim, A., Fanikos, I. A., Aristeidakis, J. S., & Haidemenopoulos, G. N. (2019). Modeling of Microsegregation and Homogenization of 6xxx Al-Alloys Including Precipitation and Strengthening During Homogenization Cooling. Materials, 12(9), 1421. https://doi.org/10.3390/ma12091421