Deposition and element fractionation processes during atmospheric pressure laser sampling for analysis by ICP-MS

被引:731
作者
Eggins, SM [1 ]
Kinsley, LPJ
Shelley, JMG
机构
[1] Australian Natl Univ, Dept Geol, GEMOC, ARC Key Ctr, Canberra, ACT 0200, Australia
[2] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia
关键词
laser ablation; LA-ICP-MS; elemental fractionation;
D O I
10.1016/S0169-4332(97)00643-0
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We have used an ArF excimer laser coupled to a quadrupole inductively coupled plasma mass spectrometry (ICP-MS) for the measurement of a range of elements during excavation of a deepening ablation pit in a synthetic glass (NIST 612). Analyte behaviour shows progressive volatile element enrichment at shallow hole depths, with a change to refractory element enrichment as the ablation pit deepens further. Examination of ablation pit morphology and the surface condensate deposited around the ablation site reveals the importance of sequential condensation of refractory. then volatile phases from the cooling plasma plume after the end of the laser pulse. We interpret the observed element fractionation behaviour to reflect a change in ablation processes from photothermal dominated to plasma dominated mechanisms. The development of the surface deposit is greatly reduced by ablating in an ambient atmosphere of ne instead of Ar and is accompanied by a two- to four-fold increase in ICP-MS sensitivity. (C) 1998 Elsevier Science B.V.
引用
收藏
页码:278 / 286
页数:9
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