Département de Chimie, Université de Sherbrooke, 2500 Boulevard Université, Sherbrooke, Québec, Canada J1K 2R1.
J Phys Chem A. 2011 Jun 16;115(23):6002-14. doi: 10.1021/jp110398j. Epub 2011 Apr 20.
Molecular beams were used to grow amorphous and crystalline H(2)O films and to dose HCl upon their surface. The adsorption state of HCl on the ice films was probed with infrared spectroscopy. A Zundel continuum is clearly observed for exposures up to the saturation HCl coverage on ice upon which features centered near 2530, 2120, 1760, and 1220 cm(-1) are superimposed. The band centered near 2530 cm(-1) is observed only when the HCl adlayer is in direct contact with amorphous solid water or crystalline ice films at temperatures as low as 20 K. The spectral signature of solid HCl (amorphous or crystalline) was identified only after saturation of the adsorption sites in the first layer or when HCl was deposited onto a rare gas spacer layer between the HCl and ice film. These observations strongly support conclusions from recent electron spectroscopy work that reported ionic dissociation of the first layer HCl adsorbed onto the ice surface is spontaneous.
分子束用于生长非晶和晶体 H(2)O 薄膜,并在其表面注入 HCl。用红外光谱法探测 HCl 在冰膜上的吸附态。在冰上的 HCl 饱和覆盖度下,清晰地观察到 Zundel 连续体,其上叠加了中心位于 2530、2120、1760 和 1220 cm(-1)附近的特征。当 HCl 吸附加层在 20 K 以下的温度下与非晶态固相水或晶态冰膜直接接触时,仅观察到中心位于 2530 cm(-1)附近的带。只有在第一层吸附位饱和后,或者当 HCl 沉积在 HCl 和冰膜之间的稀有气体间隔层上时,才会识别出固态 HCl(非晶态或晶态)的光谱特征。这些观察结果强烈支持最近电子能谱工作的结论,即报告指出吸附在冰表面的第一层 HCl 的离子离解是自发的。