NEW QUANTITATIVE APPROACH IN TRACE ELEMENTAL ANALYSIS OF SINGLE FLUIDINCLUSIONS - APPLICATIONS OF LASER-ABLATION INDUCTIVELY-COUPLED PLASMA-MASS SPECTROMETRY (LA-ICP-MS)

Citation
Am. Ghazi et al., NEW QUANTITATIVE APPROACH IN TRACE ELEMENTAL ANALYSIS OF SINGLE FLUIDINCLUSIONS - APPLICATIONS OF LASER-ABLATION INDUCTIVELY-COUPLED PLASMA-MASS SPECTROMETRY (LA-ICP-MS), Journal of analytical atomic spectrometry, 11(9), 1996, pp. 667-674
Citations number
27
Categorie Soggetti
Spectroscopy
ISSN journal
02679477
Volume
11
Issue
9
Year of publication
1996
Pages
667 - 674
Database
ISI
SICI code
0267-9477(1996)11:9<667:NQAITE>2.0.ZU;2-8
Abstract
Laser ablation inductively coupled plasma mass spectrometry has been u sed for the in situ elemental analysis of individual fluid inclusions with artificially prepared fluid inclusions as external standards. Art ificial fluid inclusions standards were prepared by drawing a standard solution of known composition into microcapillary tubes. An ICP-MS eq uipped with an Nd:YAG laser operating in the UV region (266 nm) was us ed for data acquisition. The laser was focused and bred on 25-30 mu m spots on the microcapillary tubes until the fluid was reached The cont ent of the microcapillary tube then emptied and was transported with a rgon to the torch. The average volume of fluid released, per pulse of laser, was approximately 100 pl. Calibration corves were created by pl otting signal intensity versus concentration. The long-term precision (RSD%) of measurements for Sr were 1.1-3.1% for a 1000 ppm solution, 2 .7-4.9% for a 500 ppm solution and 3.1% for a 250 ppm solution. Simila r measurements on the same solutions for Rb gave values of 1.9-2.3% fo r a 1000 ppm solution, 5.1-6.3% for a 500 ppm solution and 1.7% for a 250 ppm solution. The technique was tested on fluid inclusions in hali te from the Pale Duro Basin, Texas, USA. The results show that concent rations for Sr range from 90 to 153 ppm, and for Rb from 98 to 100 ppm . The precision of analysis for individual natural fluid inclusions ra nges from 5 to 31% for both Sr and Rb. The concentration of Sr calcula ted by this method is in agreement with earlier work.