Analysis and differentiation of mineral dust by single particle laser mass spectrometry

被引:33
|
作者
Gallavardin, Stephane [1 ]
Lohmann, Ulrike [1 ]
Cziczo, Daniel [1 ]
机构
[1] ETH, Inst Atmospher & Climate Sci, CH-8092 Zurich, Switzerland
关键词
aerosol mass spectrometry; mineralogy;
D O I
10.1016/j.ijms.2008.04.031
中图分类号
O64 [物理化学(理论化学)、化学物理学]; O56 [分子物理学、原子物理学];
学科分类号
070203 ; 070304 ; 081704 ; 1406 ;
摘要
This study evaluates the potential of single particle laser desorption/ionization mass spectrometry for the analysis of atmospherically relevant mineral dusts. Samples of hematite, goethite, calcium carbonate, calcium sulfate, silica, quartz, montmorrillonite, kaolinite, illite, hectorite, wollastonite and nephelinsyenit were investigated in positive and negative ion mode with a monopolar time-of-flight mass spectrometer where the desorption/ionization step was performed with a 193 nm excimer laser (similar to 10(9) W/cm(2)). Particle size ranged from 500 nm to 3 mu m. Positive mass spectra mainly provide elemental composition whereas negative ion spectra provide information on element speciation and of a structural nature. The iron oxide, calcium-rich and aluminosilicate nature of particles is established in positive ion mode. The differentiation of calcium materials strongly relies on the calcium counter-ions in negative mass spectra. Aluminosilicates can be differentiated in both positive and negative ion mode using the relative abundance of various aluminum and silicon ions. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:56 / 63
页数:8
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