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Reversible Phase Transformation on Ge (111) Surface by Potential

机译:Ge(111)表面上电位的可逆相变

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Reversible phase transformation on atomically flatGe (111) induced by potential in 40% NH4F solution has beenobserved with in situ scanning tunneling microscope. The abruptchange in Ge surface morphology as a function of the potential isattributed to the phase transformation, where small terraces areconverted into large terraces as the potential is changed from –1.32 to-0.98 V. Cyclic voltammograms show that the chargeunder the cathodic peak is almost the same as that under theanodic peak (4.2250L?0-4C/cm2). Combined with ex situ X-rayphotoelectron spectroscopy and secondary-ion mass spectroscopyresults, we conclude that Ge (111) surface is terminated by amonolayer hydroxide or hydride depending on the appliedpotential. The formation of hydroxide-terminated Ge (111) islikely co occur at –0.98 V, far away from the anodic peak in thecyclic voltammogram. This fact suggests that the reversible phasetransformation between monolayer hydrogen- and hydroxyl-capped Ge (111) surface is induced by potential. An atomicallyflat Ge (111) surface prepared with wet cleaning provides anattractive substrate for epitaxial growth of compound semiconductors.
机译:用原位扫描隧道显微镜观察到在40%NH4F溶液中由电势引起的原子平面Ge(111)的可逆相变。 Ge表面形貌随电位的突然变化归因于相变,当电位从–1.32 V变为-0.98 V时,小阶跃层转换为大阶跃层。循环伏安图显示,阴极峰下的电荷几乎等于与阳极峰下的相同(4.2×250L×0-4C / cm2)。结合异位X射线光电子能谱和二次离子质谱法的结果,我们得出结论,Ge(111)表面取决于所施加的电势被单层氢氧化物或氢化物封端。氢氧化物末端的Ge(111)的形成很可能在–0.98 V时发生,远离循环伏安图中的阳极峰。这一事实表明,单层氢和羟基封盖的Ge(111)表面之间的可逆相变是由电势引起的。用湿法清洁制备的原子平坦的Ge(111)表面为化合物半导体的外延生长提供了有吸引力的衬底。

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