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Seed Layers of the titania - lead oxide system

机译:二氧化钛-氧化铅系统的种子层

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Seed layers of (TiO_2)_x(PbO)_y for the growth Pb(Z,Ti)O_3 (PZT) thin films have been studied as a function of thickness and composition. The seed layers have been deposited by reactive in-situ sputter deposition at 530℃ from two metal targets in a dynamic sputtering mode. The compositional variation was achieved by varying the relative fluxes. The PZT process was run with a limited lead excess resulting in pyrochlore nucleation on bare Pt electrodes. When the electrode was covered with a dense seed layer, perovskite was obtained everywhere. Ti rich seed layers yielded (111)-textured PZT even for very thin seed layers. Pb rich seed layers nucleated as PbTiO_3 {100} and gave rise to (100)-textured PZT. In an intermediate zone, the major perovskite orientations (100), (110) and (111) have been found together with pyrochlore for a small seed layer thickness. In this zone, the seed layer nucleates in islands leaving bare Pt spots. The intermediate region is a transition region between (111) seeds and (100) seeds. The latter exhibit diverging critical sizes at a given critical flux ratio, leading to large nuclei and bare Pt. Small perovskite(111) seed grains in the 10 to 100 nm range are found at equal lead oxide and titania flux.
机译:研究了用于生长Pb(Z,Ti)O_3(PZT)薄膜的(TiO_2)_x(PbO)_y的种子层随厚度和组成的变化。种子层是通过动态溅射方式在530℃下从两个金属靶材进行反应性原位溅射沉积而形成的。组成变化是通过改变相对通量来实现的。在有限的铅过量下运行PZT工艺,导致在裸露的Pt电极上烧绿石成核。当电极上覆盖有致密的籽晶层时,到处都会得到钙钛矿。即使对于非常薄的种子层,富含Ti的种子层也可产生(111)织构的PZT。富含Pb的晶种层成核为PbTiO_3 {100},并生成(100)织构的PZT。在中间区域,发现钙钛矿的主要取向(100),(110)和(111)与烧绿石一起形成较小的种子层厚度。在该区域中,种子层在岛中成核,仅留下裸露的Pt点。中间区域是(111)种子和(100)种子之间的过渡区域。后者在给定的临界通量比下显示出不同的临界尺寸,从而导致大核和裸露的Pt。发现在相同的氧化铅和二氧化钛通量下,钙钛矿(111)晶种较小,粒径在10至100 nm之间。

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