30.01.2013 Views

Thixoforming : Semi-solid Metal Processing

Thixoforming : Semi-solid Metal Processing

Thixoforming : Semi-solid Metal Processing

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

160j 5 Thermochemical Simulation of Phase Formation<br />

Figure 5.10 Molar liquid fraction as a function of temperature for<br />

100Cr6 using equilibrium (<strong>solid</strong>), standard Scheil (dash-dotted),<br />

modified Scheil (dotted) and DICTRA (dashed) calculation.<br />

simulation. The standard Scheil calculation is completely different. The fact that the<br />

equilibrium and DICTRA curve are very close suggests that there is very little<br />

segregation, but both Mn and Cr do segregate appreciably. It is not possible to<br />

determine the liquid fraction from quenched metallographic samples in this steel [5].<br />

Figure 5.11 shows a DICTRA simulation of quenching from 50% liquid. There is only<br />

a gradual change in the composition profiles and there is no possibility of distinguishing<br />

the austenite present in the initial state from the austenite formed during<br />

quenching. Further details are given in Chapter 3.<br />

5.3.3<br />

Compositional Variations<br />

As for X210CrW12, the influence of compositional variations can be quantified in a<br />

straightforward manner. In the following, the influence of the composition on a<br />

number of key points for 100Cr6 is considered. These are linearized around the<br />

standard composition (given in Table 5.1) and given in mass%. They are roughly valid<br />

within the composition limits given by, for example, the DIN standard. The liquidus<br />

is given by:<br />

T L ¼ 1455 C 72D%C 16D%Si 4:0D%Mn 1:2D%Cr ð5:7Þ<br />

The temperature at which there is 50% liquid is given by:<br />

T 50 ¼ 1418 C 109D%C 26D%Si 5:3D%Mn 0D%Cr ð5:8Þ

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!