H.K.D.H. Bhadeshia,
Phase Transformations Group,
Department of Materials Science and Metallurgy,
University of Cambridge,
Cambridge, U.K.
Uses a finite difference method for the solution of the problem of X enrichment during the ageing of bainitic steels.
Complete program.
| Language: | FORTRAN |
| Product form: | Source code |
When cementite first forms in bainite or martensite, it grows by a paraequilibrium transformation mechanism, so substitutional solutes (such as chromium or manganese) do not partition during growth. The cementite therefore has a non-equilibrium composition when it first forms. In fact, the ratio of iron to X (substitutional solute) in the cementite is the same as that in the parent phase.
Since the cementite is not at equilibrium due to the slow diffusivity of X at low temperatures, there will be a tendency for solute to partition between the the cementite and matrix over time. MAP_STEEL_FINITE calculates this redistribution by diffusion.
None.
No information supplied.
None.
Complete program
838.15 0.5D-03 39.0D+00 2.5D+00 1.0D-07 2.0D-06 1000 5
0.0003D+00 2.0D+00 43.2 6 5 2 2
2.53D-04 240580 0
1 0.7012D+01 (Cementite)
2 0.6998D+01
3 0.6988D+01
4 0.6983D+01 Slice number, normalised conc.
5 0.6982D+01
1 0.2205D-01 (Ferrite)
2 0.4387D-01
3 0.6565D-01
4 0.8737D-01
5 0.1090D+00
6 0.1306D+00
None.
finite differences, enrichment, bainite ageing
MAP originated from a joint project of the National Physical Laboratory and the University of Cambridge.
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