Representative sampling using single-pulse laser ablation with inductively coupled plasma mass spectrometry

TitleRepresentative sampling using single-pulse laser ablation with inductively coupled plasma mass spectrometry
Publication TypeJournal Article
LBNL Report NumberLBNL-48423
Year of Publication2001
AuthorsLiu, H. C., Xianglei Mao, and Richard E. Russo
JournalJ.Anal.Atom.Spectrom.
Volume16
Pagination1115-1120
Accession Number134
Keywordsablated mass, ablation, analysis, ca, chemical analysis, chemical-analysis, composition, correlation, crater, dependence, depth, elemental fractionation, emission-spectroscopy, fractionation, glass, glass samples, glasses, icp ms, icp-ms, icpms, inductively coupled plasma, inductively coupled plasma mass spectrometry, inductively-coupled-plasma, intensities, intensity, irradiance, laser, laser ablation, laser ablation sampling, laser-ablation, mass, mass spectrometry, mass-spectrometry, measurement, measurements, nist, no, particle, pb/u, plasma, plasma mass spectrometry, plasma-mass-spectrometry, pulse, pulse laser, pulse laser ablation, ratio, sampling, segregation, signal, silicon, single, spectrometry, time, usa, volume
Abstract

Single pulse laser ablation sampling with inductively coupled plasma mass spectrometry (ICP-MS) was assessed for accurate chemical analysis. Elemental fractionation (e.g. Pb/U), the quantity of ablated mass (crater volume), ICP-MS intensity and the particle contribution (spike signal) during single pulse ablation of NIST 610 glass were investigated. Pb/U fractionation significantly changed between the first and second laser pulse and showed strong irradiance dependence. The Pb/U ratio obtained by the first pulse was usually higher than that of the second pulse, with the average value close to the representative level. Segregation during laser ablation is proposed to explain the composition change between the first and second pulse. Crater volume measurements showed that the second pulse produced significantly more ablated mass. A roll-off of the crater depth occurred at similar to 750 GW cm(-2). The absolute ICP-MS intensity from the second pulse showed no correlation with crater depth. Particle induced spikes on the transit signal showed irradiance and elemental species dependence

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