论文标题

化学解吸与能量耗散:HCO形成的Ab-Initio分子动力学的见解

Chemical desorption versus energy dissipation: insights from ab-initio molecular dynamics of HCO formation

论文作者

Pantaleone, Stefano, Enrique-Romero, Joan, Ceccarelli, Cecilia, Ugliengo, Piero, Balucani, Nadia, Rimola, Albert

论文摘要

分子云是恒星形成的银河系的冷区域。它们被相当复杂的分子丰富。这些分子中的许多分子都被认为是在渗透到星系的星际亚微米大小的尘埃晶粒的冰上表面上合成的。在10 K时,热解剂效率低下,因此,为什么在冷气中发现这些分子多年来具有诱人的天文学家。当前模型的假设(称为化学解吸)是,晶粒表面化学反应释放的分子形成能被晶粒部分吸收,其余的分子会导致新形成的分子射入气体中。在这里,我们报告了一个准确的AB-Initio分子动力学模拟,旨在研究H添加链在CO,CO + H $ \ rightarrow $ HCO上发行的能量的命运,该链在结晶冰表面模型上发生。我们表明,大约90%的HCO地层能量在第一个Picsecond中注入冰,使HCO的能量含量(10-15 kJ mol $^{ - 1} $)比其吸附能低的两个因子多(30 kj mol $ $^{ - 1} $)。结果,与实验室实验一致,我们得出结论,对于该特定系统,即晶体冰上的H + CO是无效的。我们怀疑在处理氢键时,这种行为是相当普遍的,这些氢键既是冰的粘合能和与吸附物的相互作用,因为HCO自由基,即使需要临时模拟来对其他系统得出特定的结论。

Molecular clouds are the cold regions of the Milky Way where stars form. They are enriched by rather complex molecules. Many of these molecules are believed to be synthesized on the icy surfaces of the interstellar submicron-sized dust grains that permeate the Galaxy. At 10 K thermal desorption is ineffcient and, therefore, why these molecules are found in the cold gas has tantalized astronomers for years. The assumption of the current models, called chemical desorption, is that the molecule formation energy released by the chemical reaction at the grain surface is partially absorbed by the grain and the remaining one causes the ejection of the newly formed molecule into the gas. Here we report an accurate ab-initio molecular dynamics simulations aimed to study the fate of the energy released by the first reaction of the H addition chain on CO, CO + H $\rightarrow$ HCO, occurring on a crystalline ice surface model. We show that about 90% of the HCO formation energy is injected towards the ice in the first picosecond, leaving HCO with an energy content (10-15 kJ mol$^{-1}$) more than a factor two lower than its adsorption energy (30 kJ mol$^{-1}$). As a result, in agreement with laboratory experiments, we conclude that chemical desorption is ineffcient for this specific system, namely H + CO on crystalline ice. We suspect this behavior to be quite general when dealing with hydrogen bonds, which are responsible of both the cohesive energy of the ice mantle and the interaction with adsorbates, as the HCO radical, even though ad hoc simulations are needed to draw specific conclusions on other systems.

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