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(1×1)氧覆盖的Ru(0001)上与裸Ru(0001)上的水层初始生长情况对比。

Initial growth of the water layer on (1 x 1)-oxygen-covered Ru(0001) in comparison with that on bare Ru(0001).

作者信息

Thiam Michel Malick, Kondo Takahiro, Horimoto Noriko, Kato Hiroyuki S, Kawai Maki

机构信息

RIKEN (The Institute of Physical and Chemical Research), Wako 351-0198, Japan.

出版信息

J Phys Chem B. 2005 Aug 25;109(33):16024-9. doi: 10.1021/jp052167q.

DOI:10.1021/jp052167q
PMID:16853034
Abstract

The initial growth of a water (D2O) layer on (1 x 1)-oxygen-covered Ru(0001) has been studied in comparison with that on bare Ru(0001) by means of temperature-programmed desorption (TPD) and infrared reflection absorption spectroscopy (IRAS). Although water molecules adsorbed on both bare and (1 x 1)-oxygen-covered Ru(0001) commonly tend to form hydrogen bonds with each other when mobility occurs upon heating, the TPD and IRAS measurements for the two surfaces exhibit distinct differences. On (1 x 1)-oxygen-covered Ru(0001), most of the D2O molecules were desorbed with a peak at 160 K, even at submonolayer coverage, as condensed water desorption. The vibration spectra of adsorbed D2O also showed broad peaks such as a condensed water phase, from the beginning of low coverage. For submonolayer coverage, in addition, we found a characteristic O-D stretching mode at around 2650 cm(-1), which is never clearly observed for D2O on bare Ru(0001). Thus, we propose a distinctive water adsorption structure on (1 x 1)-oxygen-covered Ru(0001) and discuss its influence on water layer growth in comparison with the case of D2O on bare Ru(0001).

摘要

通过程序升温脱附(TPD)和红外反射吸收光谱(IRAS),研究了在(1×1)氧覆盖的Ru(0001)上生长的水(D₂O)层,与在裸Ru(0001)上生长的水层进行了比较。尽管吸附在裸Ru(0001)和(1×1)氧覆盖的Ru(0001)上的水分子在加热时发生迁移时通常倾向于相互形成氢键,但两个表面的TPD和IRAS测量结果显示出明显差异。在(1×1)氧覆盖的Ru(0001)上,即使在亚单层覆盖时,大多数D₂O分子也会在160 K处出现一个脱附峰,如同冷凝水脱附。吸附的D₂O的振动光谱从低覆盖开始就显示出宽峰,如冷凝水相。此外,对于亚单层覆盖,我们在约波数2650 cm⁻¹处发现了一个特征性的O-D伸缩模式,这在裸Ru(0001)上的D₂O中从未清晰观察到。因此,我们提出了在(1×1)氧覆盖的Ru(0001)上一种独特的水吸附结构,并与裸Ru(0001)上D₂O的情况相比,讨论了其对水层生长的影响。

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