Effects of composition and growth parameters on phase formation in multicomponent aluminum garnet crystals.

Matheus Pianassola, M. Alexander, B. Chakoumakos, M. Koschan, C. Melcher, M. Zhuravleva
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Abstract

The effects of composition on the phase formation of multicomponent garnet crystals grown via directional solidification by the micro-pulling-down method are studied. A relatively wide range of rare-earth (RE) average ionic radii (AIR) is explored by formulating ten compositions from the system (Lu,Y,Ho,Dy,Tb,Gd)3Al5O12. Crystals were grown at either 0.05 or 0.20 mm min-1. The hypothesis is that multicomponent compounds with large AIR will form secondary phases as the single-RE aluminum garnets formed by larger Tb3+ or Gd3+; this will result in crystals of poor optical quality. Crystals with large AIR have a central opaque region in optical microscopy images, which is responsible for their reduced transparency compared to crystals with small AIR. Slow pulling rates suppress the formation of the opaque region in crystals with intermediate AIR. Powder and single-crystal X-ray diffraction and electron probe microanalysis results indicate that the opaque region is a perovskite phase. Scanning electron microscopy and energy dispersive spectroscopy measurements reveal eutectic inclusions at the outer surface of the crystals. The concentration of the eutectic inclusions increases with increasing AIR.
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组成和生长参数对多组分铝石榴石晶体相形成的影响。
研究了成分对微拉下定向凝固多组分石榴石晶体相形成的影响。用Lu,Y,Ho,Dy,Tb,Gd)3Al5O12体系配制了10种组分,探索了稀土(RE)平均离子半径(AIR)的较宽范围。晶体在0.05或0.20 mm min-1下生长。假设具有较大AIR的多组分化合物会像较大Tb3+或Gd3+形成的单稀土铝石榴石一样形成二次相;这将导致晶体光学质量差。具有大AIR的晶体在光学显微镜图像中有一个中心不透明区域,这是与具有小AIR的晶体相比其透明度降低的原因。缓慢的拉速抑制了中间气相晶体中不透明区域的形成。粉末和单晶x射线衍射及电子探针显微分析结果表明,不透明区为钙钛矿相。扫描电子显微镜和能量色散光谱测量显示晶体外表面有共晶夹杂物。共晶夹杂的浓度随空气浓度的增加而增加。
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