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人工雪颗粒表面上的 1-甲基萘的自组织:一种组合实验计算方法。

Self-organization of 1-methylnaphthalene on the surface of artificial snow grains: a combined experimental-computational approach.

机构信息

Department of Chemistry, Faculty of Science, Masaryk University, Brno, Czech Republic.

出版信息

J Phys Chem A. 2011 Oct 20;115(41):11412-22. doi: 10.1021/jp205627a. Epub 2011 Sep 1.

DOI:10.1021/jp205627a
PMID:21882845
Abstract

A combined experimental-computational approach was used to study the self-organization and microenvironment of 1-methylnaphthalene (1MN) deposited on the surface of artificial snow grains from vapors at 238 K. The specific surface area of this snow (1.1 × 10(4) cm(2) g(-1)), produced by spraying very fine droplets of pure water from a nebulizer into liquid nitrogen, was determined using valerophenone photochemistry to estimate the surface coverage by 1MN. Fluorescence spectroscopy at 77 K, in combination with molecular dynamics simulations, and density functional theory (DFT) and second-order coupled cluster (CC2) calculations, provided evidence for the occurrence of ground- and excited-state complexes (excimers) and other associates of 1MN on the snow grains' surface. Only weak excimer fluorescence was observed for a loading of 5 × 10(-6) mol kg(-1), which is ∼2-3 orders of magnitude below monolayer coverage. However, the results indicate that the formation of excimers is favored at higher surface loadings (>5 × 10(-5) mol kg(-1)), albeit still being below monolayer coverage. The calculations of excited states of monomer and associated moieties suggested that a parallel-displaced arrangement is responsible for the excimer emission observed experimentally, although some other associations, such as T-shape dimer structures, which do not provide excimer emission, can still be relatively abundant at this surface concentration. The hydrophobic 1MN molecules, deposited on the ice surface, which is covered by a relatively flexible quasi-liquid layer at 238 K, are then assumed to be capable of dynamic motion resulting in the formation of energetically preferred associations to some extent. The environmental implications of organic compounds' deposition on snow grains and ice are discussed.

摘要

采用实验-计算相结合的方法研究了萘(1MN)在 238 K 下从蒸汽沉积在人工雪颗粒表面的自组织和微环境。使用苯乙酮光化学法来估计 1MN 的表面覆盖率,确定了这种雪(1.1×10^4 cm^2 g^-1)的比表面积,这种雪是通过将纯水的非常细的液滴喷射到液氮中制成的。在 77 K 下进行荧光光谱学研究,结合分子动力学模拟和密度泛函理论(DFT)和二级耦合簇(CC2)计算,为在雪颗粒表面发生基态和激发态复合物(激基复合物)和 1MN 的其他配合物提供了证据。在 5×10^-6 mol kg^-1 的负载下,仅观察到微弱的激基复合物荧光,这大约是单层覆盖的 2-3 个数量级。然而,结果表明,在更高的表面负载(>5×10^-5 mol kg^-1)下,激基复合物的形成更有利,尽管仍低于单层覆盖。单体和相关部分的激发态的计算表明,实验中观察到的激基复合物发射是由平行位移排列负责的,尽管一些其他的配合物,如 T 型二聚体结构,不会提供激基复合物发射,但在这个表面浓度下仍可能相对丰富。假设在 238 K 下,疏水的 1MN 分子沉积在冰表面上,冰表面覆盖着相对灵活的准液态层,然后可以进行动态运动,从而在一定程度上形成能量上优先的配合物。讨论了有机化合物在雪颗粒和冰上沉积的环境影响。

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