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Reactive wetting of rutile by liquid aluminium

机译:液态铝对金红石的反应性润湿

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摘要

Sessile drop wetting experiments of liquid Al on polycrystalline rutile (TiO2) were conducted in the 973.1273 K temperature range under a low total pressure (9.3 10.3 Pa, Ar) and a low oxygen partial pressure (Ŝ 1.33 10.7 Pa), as a function of temperature and time. A non-wetting (150., 973 K, t >120 min.) to partial wetting (85., 1273 K, 50.60 min.) transition reflects reactive wetting characteristics. Microstructural investigations of the metal-ceramic interface shows that TiO2 is reduced by liquid Al, resulting in the formation of Al2O3. The steady-state contact angle at 1273 K of Al on α-Al2O3 and Al on rutile are very similar, and the role of Ti segregation is minimal. It appears that spreading of the Al drop on TiO2 is governed by the reduction reaction at the solid-liquid interface. The measured activation energy corresponds well to the activation energy for volume diffusion of Al, Ti and O in rutile and the volume diffusion of Al in polycrystalline α-Al2O3.
机译:液态Al在多晶金红石(TiO2)上的无滴润湿实验是在973.1273 K温度范围内,低总压(9.3 10.3 Pa,Ar)和低氧分压(Ŝ1.33 10.7 Pa)下进行的,温度和时间。从非润湿(150.,973 K,t> 120分钟)到部分润湿(85.,1273 K,50.60分钟)的转变反映了反应性润湿特性。对金属-陶瓷界面的微观结构研究表明,液态铝将TiO2还原,从而形成Al2O3。 Al在α-Al2O3上的Al和金红石上的Al在1273 K处的稳态接触角非常相似,并且Ti偏析的作用很小。看来,Al滴在TiO2上的扩散受固液界面处的还原反应支配。测得的活化能与金红石中Al,Ti和O的体积扩散以及多晶α-Al2O3中Al的体积扩散的活化能非常吻合。

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  • 来源
    《Journal of Materials Science》 |2005年第5期|1093-1100|共8页
  • 作者

    S. Avraham; W. D. Kaplan;

  • 作者单位

    Department of Materials Engineering Technion-Israel Institute of Technology;

    Department of Materials Engineering Technion-Israel Institute of Technology;

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  • 正文语种 eng
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