P_15: Smooth Transition from Paraequilibrium to Ortho-equilibrium
In this example, the precipitation of cementite during tempering of an Fe-Mn-C steel is simulated considering three interface conditions: the usual ortho-equilibrium (OE) condition; paraequilibrium (PE) condition; and a smooth transition from paraequilibrium to ortho-equilibrium condition (PE-OE). The simulation results are compared with the experimental data from Miyamoto et al. [2007Miy].
The Precipitation Calculator nodes are renamed in the example to match the abbreviations for the three interface conditions considered: OE, PE, and PE-OE. Also see the video to learn how to create this example.
This example demonstrates that the early stage of the cementite precipitation follows a PE condition, under which the precipitation kinetics is controlled by the diffusion of C. At a later stage, gradual transition from PE condition to OE condition occurs, and if the tempering time is long enough the diffusion of Mn has a dominating effect on the coarsening of cementite. While a Simplified model follows the OE condition and a Para-eq model follows PE condition, the PE Automatic model enables the smooth transition from PE condition at early stage to OE condition at a late stage.
The example uses the demonstration steel databases, FEDEMO and MFEDEMO. These databases are available to all users (i.e. you do not need a license for the Precipitation Module (TC-PRISMA)) and contain the necessary thermodynamic and kinetic data needed for the calculation.
For more details, see PE Automatic Growth Rate Model described in the Growth theory section.

- Folder: Precipitation Module - TC-PRISMA
- File name:
P_15_Precipitation_Fe-C-Mn_PE-OE_Precipitation_of_Cementite.tcu
Example Settings
System (System Definer) | |
Database package | Demo: Steels and Fe-alloys (FEDEMO and MFEDEMO) |
Elements | Fe, Mn, C |
Conditions (Precipitation Calculator) | |
Composition |
Fe-1.96Mn-0.61C mass percent |
Matrix phase |
BCC_A2 Click Show Details:
All other defaults are kept. |
Precipitate phase |
CEMENTITE_D011 Click Show Details to select the Growth rate model (Simplified, Para-eq, and PE Automatic). All other defaults are kept. |
Calculation Type (Precipitation Calculator) | |
Calculation type | Isothermal |
Temperature | 923.15 Kelvin |
Simulation time |
1E6 seconds for Simplified and PE Automatic models, and 5 seconds for Para-eq model |
Datasets (Experimental File Reader) | |
Mean Radius Exp | Data set including experimental mean radius of cementite |
Mn Concentration | Data set including experimental Mn composition in cementite |
Visualizations
This example is included as a Precipitation Module (TC-PRISMA) tutorial on our website and as part of the playlist on our YouTube channel.
Open the example project file to review the node setup on the Project window and the associated settings on the Configuration window for each node. For some types of projects, you can also adjust settings on the Plot Renderer Configuration window to preview results before performing the simulation. Click Perform Tree to generate plots and tables to see the results on the Visualizations window.
When you run (Perform) this example, it takes a few minutes for the calculations to complete.
There is a variety of information shown in the Visualizations window that can be viewed during configuration and after performing the calculation.
- Thermal Profile: When setting up a calculator on a Configuration window for Isothermal or Non-isothermal Calculation Types, you can preview the profile and adjust settings as needed. When you click a calculator node in the Project window, the matching name of the node is on the tab(s) displayed in the Visualizations window.
For TTT Diagram and CCT Diagram calculations there is nothing shown for the Precipitation Calculator tab in the Visualizations window as there is no Thermal Profile to be defined.
- Plot or Table results: After completing the set up and performing the calculation, to view the matching name of the node on tab(s) in the Visualizations window, either click a Plot Renderer or Table Renderer node in the Project window or click the tabs individually in the Visualizations window.
For this Isothermal example, its Thermal Profile is also displayed in the Visualizations window showing the constant temperature entered for this calculation type. The tab names match the node names in the Project window.
Figure 1: A comparison between the measurements of mean cementite radius from [2007Miy] with the simplified (OE), para-eq (PE), and PE Automatic (PE-OE) growth models. The PE-OE model is needed to capture the nucleation, growth, and coarsening behavior of cementite.
Figure 2: A comparison of the evolution of the cementite Mn composition during isothermal aging at 923.15 K between the experimental data from [2007Miy] with model predictions obtained from the simplified (OE) growth model, the para-eq (PE) growth model, and the PE Automatic (PE-OE) growth model. The PE-OE model captures the behavior shown in the experimental data, where the Mn composition transitions from the initial ferrite composition towards the equilibrium cementite composition.
Reference
[2007Miy] G. Miyamoto, J. Oh, K. Hono, T. Furuhara, T. Maki, Effect of partitioning of Mn and Si on the growth kinetics of cementite in tempered Fe–0.6 mass% C martensite. Acta Mater. 55, 5027–5038 (2007).