R. Dupuy, M. Haubner, B. Henrist, J. Fillion, V. Baglin
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引用次数: 6
摘要
表面冷冻吸附分子的电子刺激解吸(ESD)是一个与加速器真空动力学和天体化学等领域相关的过程。虽然由keV电子和快离子诱导的分子系统的脱附已经被广泛研究,但亚keV电子的机制相对来说鲜为人知。在150 ~ 2000 eV的电子能范围内,对分子冰体系(N$_2$, CO$_2$, CO$_2$, Ar $和H$_2$O/D$_2$O)的电子激发解吸进行了测量和量化。在这种情况下,停止功率不再足以解释ESD产量的电子能量依赖性。我们引入了解吸相关深度的概念,它表征了地表附近两种能量沉积机制之间的转变。然后,我们将这一概念应用于不同的系统,展示了亚kev状态下的ESD如何揭示晶体和多孔非晶CO$_2$冰中物质扩散的差异。
Electron-stimulated desorption from molecular ices in the 0.15–2 keV regime
Electron-stimulated desorption (ESD) of cryosorbed molecules on surfaces is a process of relevance to fields as varied as vacuum dynamics in accelerators and astrochemistry. While desorption from such molecular systems induced by keV electrons and fast ions has been extensively studied, the sub-keV electron regime is comparatively little known. We measured and quantified electron-stimulated desorption from molecular ice systems (layers of N$_2$, CO, CO$_2$, Ar and H$_2$O/D$_2$O condensed at cryogenic temperatures) in the 150-2000 eV electron energy range. In this regime stopping power is no longer sufficient to explain the electron energy dependence of ESD yields. We introduce the notion of desorption-relevant depth, which characterizes the transition between two energy deposition regimes near the surface. We then apply this notion to the different systems, showing how ESD in the sub-keV regime can for example reveal the differences in species diffusion in crystalline and porous amorphous CO$_2$ ices.