Dipartimento Scienze Geologiche, Università Roma Tre, 00146 Roma, Italy.
Anal Bioanal Chem. 2010 Jul;397(6):2039-49. doi: 10.1007/s00216-010-3811-8. Epub 2010 May 28.
In this paper we describe recent applications of micro-infrared imaging in the Earth sciences. We address, in particular, the use of Fourier-transform infrared (FTIR) spectroscopy in characterizing the zoning and speciation of H and C in a variety of geological materials, including microporous minerals, nominally anhydrous volcanic minerals (NAMs), and crystal inclusions. These investigations show that use of the modern techniques of FTIR imaging enables detection of the zoning of volatile species across the studied samples, and possible configuration changes of structurally-bound carbon molecular species (e.g., CO(2) vs CO(3)) during crystal growth. Such features, which are not accessible with other micro-analytical techniques, may provide information about the physicochemical properties which act as constraints in the genesis of the samples, and important information about the evolution of the geological system. Tests performed with focal-plane-array detectors (FPA) show that resolution close to the diffraction limit can be achieved if the amounts of the target molecules in the sample are substantially different. We also point out the possibility of using FTIR imaging for investigations under non-ambient conditions.
本文介绍了微红外成像技术在地球科学中的最新应用。我们特别讨论了傅里叶变换红外(FTIR)光谱在表征各种地质材料中 H 和 C 的分带和形态方面的应用,这些地质材料包括微孔矿物、名义上无水的火山矿物(NAM)和晶体包裹体。这些研究表明,现代的 FTIR 成像技术可以检测到研究样品中挥发性物质的分带,以及在晶体生长过程中结构结合的碳分子形态(例如 CO(2) 与 CO(3))可能发生的构型变化。这些特征是其他微分析技术无法获得的,它们可能提供有关在样品成因中起约束作用的物理化学性质的信息,以及有关地质系统演化的重要信息。使用焦平面阵列探测器(FPA)进行的测试表明,如果样品中目标分子的数量存在显著差异,则可以实现接近衍射极限的分辨率。我们还指出了在非环境条件下使用 FTIR 成像进行研究的可能性。