ISSN:
1573-4803
Source:
Springer Online Journal Archives 1860-2000
Topics:
Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
Notes:
Abstract A study has been performed of the oxidation and degassing processes of aluminium-based alloy powders. Oxidation and hydration of gas-atomized metal powders take place during inflight solidification and cooling to room temperature, during collection and keeping in the powder collection box and during transport and storage before consolidation. Under the atomizing conditions, oxidation cannot be prevented. In contact with humid gases (air) the oxide layer on the powder surface takes up water vapour which is physically or chemically bound. A literature study shows that the oxide layer on atomized aluminium powder is amorphous and has a thickness of 2–10 nm depending on the atomizing conditions. The amount of water in the powder is sufficient to form a completely closed hydroxide layer on the outer surface of the powder. The thickness growth of the oxide layer is governed by cation diffusion. Degassing experiments were carried out by heating canned powders in vacuum. The partial pressures of evolved water vapour and hydrogen were registered as a function of temperature at a constant heating rate. Two different alloy powders were used: the first air atomized and containing 1% magnesium (Al-20Si-3Cu-1Mg-5Fe), and the second (Al-9Fe-2Mo-1Zr) magnesium-free powder, atomized by nitrogen. Much work has been done on degassing, but most of it is directed towards industrial applications. The quantitative theoretical description of the degassing phenomenon is still lacking. A new approach aiming at narrowing this gap is presented by employing Wagner's theory of high temperature oxidation of metals. The diffusion coefficient of aluminium cations through the amorphous aluminium oxide layer has been determined in the degassing temperature range by using the experimental data of Hayden et al. The diffusion coefficient of aluminium cations through the Al2O3 layer has also been evaluated from the degassing experiments. The values obtained directly from the degassing experiments are in reasonable agreement with those derived from the oxidation results. It has been concluded that extrapolation of the results obtained from diffusion experiments at high temperatures in aluminium oxides towards the temperature range of degassing cannot explain the formation of hydrogen during this process, even if the surface diffusion coefficient (much higher than lattice diffusion coefficient) is taken into account.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF00540704
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