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利用共振两步激光烧蚀和电离质谱法研究多组分冰中的羽流成分与演化。

Plume composition and evolution in multicomponent ices using resonant two-step laser ablation and ionization mass spectrometry.

作者信息

Henderson Bryana L, Gudipati Murthy S

机构信息

Science Division, Jet Propulsion Laboratory, California Institute of Technology , Pasadena, California 91109, United States.

出版信息

J Phys Chem A. 2014 Jul 24;118(29):5454-63. doi: 10.1021/jp503111k. Epub 2014 Jul 9.

Abstract

The composition and evolution of plumes generated in a resonant infrared (IR) laser desorption of low-temperature ices is investigated via a recently developed two-step laser desorption and ionization mass spectrometry (2S-LAIMS) technique where a neutral plume is ejected by an IR laser pulse and ionized by a UV laser pulse for analysis via time-of-flight mass spectrometry. By varying the delay between the lasers, we can construct a complete time-resolved model of the ejected plume components. We found that water ices containing mixtures of polar and nonpolar analytes displayed complex mass spectral profiles that varied as the plume evolved. In these samples, the low-volatility polar analytes and clusters were restricted to the early part of the plume, whereas volatile or nonpolar analytes were spread throughout the plume. The distributions of low-volatility polar species, clusters, and impurities from the copper substrate were well-represented by single Maxwell-like distributions centered at high velocities (600-800 m s(-1)), while nonpolar, volatile species contained two distinct components, indicating both ablation and thermal desorption processes. Characterization of plume distributions can therefore provide new insight into an analyte's chemical identity and can aid in assignment of otherwise ambiguous signals in the mass spectra.

摘要

通过最近开发的两步激光解吸和电离质谱(2S-LAIMS)技术,研究了低温冰的共振红外(IR)激光解吸中产生的羽流的组成和演化。在该技术中,中性羽流由红外激光脉冲喷射出,并由紫外激光脉冲电离,以便通过飞行时间质谱进行分析。通过改变激光之间的延迟,我们可以构建喷射羽流成分的完整时间分辨模型。我们发现,含有极性和非极性分析物混合物的水冰显示出复杂的质谱图,其随羽流演化而变化。在这些样品中,低挥发性极性分析物和团簇局限于羽流的早期部分,而挥发性或非极性分析物则遍布整个羽流。来自铜衬底的低挥发性极性物质、团簇和杂质的分布可以用以高速(600 - 800 m s(-1))为中心的单一麦克斯韦分布很好地表示,而非极性、挥发性物质包含两个不同的成分,表明存在烧蚀和热解吸过程。因此,羽流分布的表征可以为分析物的化学特性提供新的见解,并有助于识别质谱中其他模糊的信号。

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