TY - JOUR
T1 - Chemical characterization of a chromitite reference sample GPt-5 using INAA and ICP-MS
AU - Akhter, Rabeya
AU - Shirai, Naoki
AU - Ebihara, Mitsuru
N1 - Funding Information:
Rabeya Akhter acknowledges the Asian Human Resources Fund from the Tokyo Metropolitan Government for her stay at Tokyo Metropolitan University as a Ph.D. student. This work is financially supported in part by Grant-in-Aid for Scientific Research (A) (KAKENHI) defrayed by the Japan Society for the Promotion of Science (No. 25246038 to ME).
PY - 2016
Y1 - 2016
N2 - New major, minor, and trace element (Mg, Al, Ca, Sc, V, Cr, Mn, Fe, Co, Ni, Zn, and Ir) abundances for a chromitite reference sample, GPt-5, were obtained using instrumental neutron activation analysis (INAA), and are presented in this report. Replicate analyses of GPt-5 with sample masses ranging from 22 to 64 mg showed a precision of less than 8% (1 s) for most elements, except for Ca and Ir, implying that a small amount of the GPt-5 sample (22 to 64 mg) is enough to obtain representative elemental abundances with the exception of these two elements. The large variation (44.5% for 1 s) observed in the abundance of Ir was attributed to sample heterogeneity. By using isotope dilution inductively-coupled plasma mass spectrometry (ICP-MS) coupled with NiS fire-assay pre-concentration, the concentrations of the platinum group elements (PGE; Ru, Rh, Pd, Os, Ir, and Pt) were determined for the sample powders previously used for the INAA to avoid the sampling bias in assessing the effectiveness of the NiS fire-assay digestion. It was possible to determine the abundance of Ir using both the INAA and ICP-MS, and the values obtained were consistent with each other within the measurement precision. This approach confirmed that the NiS fire-assay procedure applied in this study can digest chromite and that the accurate determination of PGE for chromite-containing rocks can be performed by using our analytical method. Based on the Ru/Rh ratio, the GPt-5 chromitite reference sample was classified as a podiform chromitite.
AB - New major, minor, and trace element (Mg, Al, Ca, Sc, V, Cr, Mn, Fe, Co, Ni, Zn, and Ir) abundances for a chromitite reference sample, GPt-5, were obtained using instrumental neutron activation analysis (INAA), and are presented in this report. Replicate analyses of GPt-5 with sample masses ranging from 22 to 64 mg showed a precision of less than 8% (1 s) for most elements, except for Ca and Ir, implying that a small amount of the GPt-5 sample (22 to 64 mg) is enough to obtain representative elemental abundances with the exception of these two elements. The large variation (44.5% for 1 s) observed in the abundance of Ir was attributed to sample heterogeneity. By using isotope dilution inductively-coupled plasma mass spectrometry (ICP-MS) coupled with NiS fire-assay pre-concentration, the concentrations of the platinum group elements (PGE; Ru, Rh, Pd, Os, Ir, and Pt) were determined for the sample powders previously used for the INAA to avoid the sampling bias in assessing the effectiveness of the NiS fire-assay digestion. It was possible to determine the abundance of Ir using both the INAA and ICP-MS, and the values obtained were consistent with each other within the measurement precision. This approach confirmed that the NiS fire-assay procedure applied in this study can digest chromite and that the accurate determination of PGE for chromite-containing rocks can be performed by using our analytical method. Based on the Ru/Rh ratio, the GPt-5 chromitite reference sample was classified as a podiform chromitite.
KW - Chromitite reference sample
KW - GPt-5
KW - Instrumental neutron activation analysis
KW - Isotope dilution inductively coupled plasma mass spectrometry
KW - NiS fire-assay
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U2 - 10.2343/geochemj.2.0403
DO - 10.2343/geochemj.2.0403
M3 - Article
AN - SCOPUS:84962779408
SN - 0016-7002
VL - 50
SP - 179
EP - 185
JO - Geochemical Journal
JF - Geochemical Journal
IS - 2
ER -