Titanium Isotope Analysis of Igneous Reference Materials using a Double‐spike MC‐ICP‐MS Method

Ti separation was achieved by ion‐exchange chromatography using Bio‐Rad AG 1‐X8 anion‐exchange and DGA resins. For high‐Fe/Ti and high‐Mg/Ti igneous samples, a three‐column procedure was required, whereas a two‐column procedure was used for low‐Fe/Ti and low‐Mg/Ti igneous samples. The Ti isotopes we...

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Bibliographic Details
Published in:Acta geologica Sinica (Beijing) 2022-04, Vol.96 (2), p.517-524
Main Authors: LI, Jin, TANG, Suohan, ZHU, Xiangkun, MA, Jianxiong, ZHAO, Xinmiao
Format: Article
Language:English
Subjects:
Anion exchanging
Anions
Calcium
Chromatography
Composition
double‐spike
Iron
Isotopes
Magnesium
mass bias correction
MC‐ICP‐MS
Molybdenum
Procedures
reference material
Reference materials
Resins
Sodium
Ti isotope
Titanium
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Summary:Ti separation was achieved by ion‐exchange chromatography using Bio‐Rad AG 1‐X8 anion‐exchange and DGA resins. For high‐Fe/Ti and high‐Mg/Ti igneous samples, a three‐column procedure was required, whereas a two‐column procedure was used for low‐Fe/Ti and low‐Mg/Ti igneous samples. The Ti isotopes were analysed by MC‐ICP‐MS, and instrumental mass bias was corrected using a 47Ti‐49Ti double‐spike technique. The 47Ti‐49Ti double‐spike and SRM 3162a were calibrated using SRM 979‐Cr, certificated value 53Cr/52Crtrue = 0.11339. Isobaric interference was evaluated by analysing Alfa‐Ti doped with Na, Mg, Ca, and Mo, and results indicate that high concentrations of Na and Mg have no significant effect on Ti isotope analyses; however, Ca and Mo interferences lead to erroneous δ49/47Ti values when Ca/Ti and Mo/Ti ratios exceed 0.01 and 0.1, respectively. Titanium isotopic compositions were determined for 12 igneous reference materials, BCR‐2, BHVO‐2, GBW07105, AGV‐1, AGV‐2, W‐2, GBW07123, GBW07126, GBW07127, GBW07101, JP‐1, and DTS‐2b. Samples yield δ49/47Ti (‰) of −0.035 ± 0.022, −0.038 ± 0.031, 0.031 ± 0.022, 0.059 ± 0.038, 0.044 ± 0.037, 0.000 ± 0.015, 0.154 ± 0.044, −0.044 ± 0.018, 0.010 ± 0.022, 0.064 ± 0.043, 0.169 ± 0.034, and −0.047 ± 0.025 (relative to OL‐Ti, ±2SD), respectively; of which isotopic compositions of DTS‐2b, JP‐1, GBW07101, GBW07105, GBW07123, GBW07126, and GBW07127 are reported for the first time. Standard Alfa‐Ti was analysed repeatedly over a ten‐month period, indicating a reproducibility of ±0.047 (2SD) for δ49/47Ti, similar to the precisions obtained for geochemical reference materials.
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.14728