Accurate determinations of fifty-four major and trace elements in carbonate by LA–ICP-MS using normalization strategy of bulk components as 100
Here we describe an internal standard-independent calibration strategy for LA–ICP-MS analysis of fifty-four major and trace elements in carbonate. Based on the normalization strategy of bulk components as 100%, the MRM-NoIS (calibrated against multiple silicate reference materials without using inte...
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Veröffentlicht in: | Chemical geology 2011-05, Vol.284 (3), p.283-295 |
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Sprache: | eng |
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Zusammenfassung: | Here we describe an internal standard-independent calibration strategy for LA–ICP-MS analysis of fifty-four major and trace elements in carbonate. Based on the normalization strategy of bulk components as 100%, the
MRM-NoIS (calibrated against multiple silicate reference materials without using internal standard) was used to correct the matrix-dependent absolute amount of materials ablated during each run. Applying
MRM-NoIS and using the MPI-DING reference glasses as reference materials for external calibration, analyses of carbonate standard MACS-3 generally agree with recommended values within 10% for most trace elements (better than 5% for REEs and major elements). Analyses of natural igneous calcite grains agree with the results of solution-ICP-MS values within 10% for Mg, Sc, Mn, Sr and REEs. The results indicate that, applying
MRM-NoIS and using MPI-DING reference glasses as multiple reference materials for calibration, carbonate can be accurately analyzed in situ by LA–ICP-MS without applying internal standardization and matrix matching external standards. Our results also indicate that the working value of Nb in carbonate pellet MACS-3 could be 53.4
μg/g rather than 35.2
μg/g given in the test of G-Probe 4.
► Applying multiple silicate reference materials without using internal standard. ► Major and trace elements in carbonate can be accurately analyzed by LA–ICP-MS. ► Working value of Nb in carbonate pellet MACS-3 is revised to be 53.4 ppm. |
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ISSN: | 0009-2541 1872-6836 |
DOI: | 10.1016/j.chemgeo.2011.03.007 |