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Thixoforming : Semi-solid Metal Processing

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290j 8 Tool Technologies for Forming of <strong>Semi</strong>-<strong>solid</strong> <strong>Metal</strong>s<br />

Figure 8.44 XRD spectra of the contact zone of Si3N4/X210CrW12 contact corrosion at 1300 C/2 h.<br />

The above-mentioned reactions are superimposed by chemical interaction with<br />

steel and scale in the areas in contact to steel. On top of the SiO2 layer a thick scale<br />

layer is observed under oxidizing conditions, consisting of ferrous oxides with<br />

varying amounts of chromium in <strong>solid</strong> solution. XRD analysis of this layer yields<br />

magnetite, haematite and chromite as major constituents in addition to cristobalite<br />

(Figure 8.44).<br />

Enclosed in this layer metallic precipitations are detected that exhibit a high<br />

amount of steel alloying elements, for example, chromium, manganese and tungsten,<br />

significantly exceeding the element content of the respective steel grade applied.<br />

Thus, alloying elements are mobilized in the bulk of the steel and diffuse to the<br />

contact zone. The entire scale layer is permeated by channels, cracks and pores<br />

resulting from the nitrogen gas released during decomposition of Si3N4 trying to<br />

escape from the contact zone.<br />

As expected, chemical interaction of Si3N4 and steel in an argon atmosphere differs<br />

from the behaviour in air: depletion of the grain boundary phase in the upper Si3N4<br />

layers is less pronounced. Likewise, precipitations containing a high amount of the<br />

sintering additive elements Yand Al are observed only locally in the contact zone. On<br />

top of the Si3N4 ceramic a metallic layer is detected, consisting mainly of iron and<br />

silicon. Embedded in this layer metallic precipitations are found, showing high<br />

amounts of steel alloying elements, and also large pores that are ascribed to the<br />

nitrogen gas emerging during decomposition of Si3N4. Although this gas can readily<br />

escape from the contact zone through the powdery and brittle scale layer in the case of<br />

oxidizing conditions, the lack of such a layer in an argon atmosphere leads to<br />

entrapment of the gas in the contact zone, eventually resulting in very large cavities<br />

formed due to the gas pressure. While more pronounced in an argon atmosphere,<br />

interdiffusion of silicon and iron is observed independently of the experimental<br />

parameters.<br />

Examination of silicon nitride die parts after application in small-scale forming<br />

series revealed that under real thixoforming conditions a combination of the<br />

aforementioned mechanisms observed in model tests in air and in an argon<br />

atmosphere is present. Although the inner die surfaces showed a mirror finish

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