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Vacuum ultraviolet photodissociation and surface morphology change of water ice films dosed with hydrogen chloride

机译:氯化氢注入水冰膜的真空紫外光解离和表面形貌变化。

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Time-of-flight(TOF)spectra of photofragment H atoms from the photodissociation of water ice films at 193 nm were measured for amorphous and polycrystalline water ice films with and without dosing of hydrogen chloride at 100-145 K.The TOF spectrum is sensitive to the surface morphology of the water ice film because the origin of the H atom is the photodissociation of dimerlike water molecules attached to the ice film surfaces.Adsorption of HCl on a polycrystalline ice film was found to induce formation of disorder regions on the ice film surface at 100-140 K,while the microstructure of the ice surface stayed of polycrystalline at 145 K with adsorption of HCl.The TOF spectra of photofragment Cl atoms from the 157 nm photodissociation of neutral HCl adsorbed on water ice films at 100-140 K were measured.These results suggest partial dissolution of HCl on the ice film surface at 100-140 K.
机译:测量了在100-145 K下有无氯化氢的无定形和多晶水冰膜在193 nm处水冰膜的光解离所产生的光碎片H原子的飞行时间(TOF)光谱.TOF光谱很敏感氢原子的起源是附着在冰膜表面的二聚体状水分子的光解离,从而导致水冰膜的表面形貌变化。发现HCl在多晶冰膜上的吸附会诱导冰膜上形成无序区域100-140 K时冰表面的微结构保持在145 K上,并有HCl吸附。在157 nm处中性HCl在100-140 K时光解离的中性HCl光解157 Cl的TOF光谱这些结果表明在100-140 K时HCl在冰膜表面部分溶解。

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