![[MAP Logo]](../../maplogo1.gif) 
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.
MAP Website administration / map@msm.cam.ac.uk