The analytical capabilities of laser ablation (LA)-ICP-AAS in determining Li, Be and B at trace levels in geological samples have been tested on a series of glass reference materials and natural samples. The LA-ICP-MS instrument used consisted of a sector-field ICP-MS coupled with a laser ablation microprobe operating at either 266 or 213 nm wavelength. Reference glasses from NIST (SRM 612, 614 and 616) and MPI-DING (KL2-G, MOB-G, StHs6/80-G, GOR128-G, GOR132-G, T1-G and ATHO-G) were selected to develop the analytical method and to assess the best instrumental configuration. A series of calcic amphiboles with different Li, Be and B concentrations were also analysed using both LA-ICP-MS and SIMS to test the applicability of the method to natural minerals. Results indicated that with a spot size of 40 mu m the agreement between measured and reference values of Li, Be and B is generally better than 10% for NIST SRM 612 and 20% for NIST SRM 614. Average reproducibility at the 2s level was 10% for Li, 20% for Be and 15% for B. Limits of detection were approximately 100 ng g(-1) for Be and B and 200 ng g(-1) for Li. These results were confirmed by analyses carried out on natural amphiboles and compared well in terms of precision and accuracy with those commonly achieved by SIMS.

Determination of lithium, beryllium and boron at trace levels by laser ablation-inductively coupled plasma-sector field mass spectrometry / M. Tiepolo, A. Zanetti, R. Vannucci. - In: GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS. - ISSN 0150-5505. - 29:2(2005), pp. 211-224. [10.1111/j.1751-908X.2005.tb00893.x]

Determination of lithium, beryllium and boron at trace levels by laser ablation-inductively coupled plasma-sector field mass spectrometry

M. Tiepolo
;
2005

Abstract

The analytical capabilities of laser ablation (LA)-ICP-AAS in determining Li, Be and B at trace levels in geological samples have been tested on a series of glass reference materials and natural samples. The LA-ICP-MS instrument used consisted of a sector-field ICP-MS coupled with a laser ablation microprobe operating at either 266 or 213 nm wavelength. Reference glasses from NIST (SRM 612, 614 and 616) and MPI-DING (KL2-G, MOB-G, StHs6/80-G, GOR128-G, GOR132-G, T1-G and ATHO-G) were selected to develop the analytical method and to assess the best instrumental configuration. A series of calcic amphiboles with different Li, Be and B concentrations were also analysed using both LA-ICP-MS and SIMS to test the applicability of the method to natural minerals. Results indicated that with a spot size of 40 mu m the agreement between measured and reference values of Li, Be and B is generally better than 10% for NIST SRM 612 and 20% for NIST SRM 614. Average reproducibility at the 2s level was 10% for Li, 20% for Be and 15% for B. Limits of detection were approximately 100 ng g(-1) for Be and B and 200 ng g(-1) for Li. These results were confirmed by analyses carried out on natural amphiboles and compared well in terms of precision and accuracy with those commonly achieved by SIMS.
light lithophile elements; laser ablation; sector field ICP-MS; MPI-DING; NIST SRM glasses
Settore GEO/08 - Geochimica e Vulcanologia
2005
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/319228
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