論文

査読有り
2017年4月

Precise isotope analysis of sub-nanogram lead by total evaporation thermal ionization mass spectrometry (TE-TIMS) coupled with a204Pb-207Pb double spike method

Journal of Analytical Atomic Spectrometry
  • Yusuke Fukami
  • ,
  • Minato Tobita
  • ,
  • Tetsuya Yokoyama
  • ,
  • Tomohiro Usui
  • ,
  • Ryota Moriwaki

32
4
開始ページ
848
終了ページ
857
記述言語
掲載種別
研究論文(学術雑誌)
DOI
10.1039/c6ja00455e

© The Royal Society of Chemistry. We present a new analytical technique for precise isotope measurement of sub-nanograms of Pb by total evaporation thermal ionization mass spectrometry (TE-TIMS) coupled with a204Pb-207Pb double spike. The precise determination of Pb isotopic composition with a small (sub-nanograms) quantity of Pb is hampered due to the low signal intensity of204Pb+, which has the lowest isotope abundance in natural samples (1.4%). The advantage of TE-TIMS is that the measured signal intensities are larger and the measurement time is shorter than those by the measurement with constant filament current. In this study, we investigated optimization of the analytical protocol for Pb isotope measurement by TE-TIMS coupled with a204Pb-207Pb double spike, including the sample loading technique, filament temperature control, and the reduction method of isotope data acquired. The Pb isotope analysis was performed with the heating rate of 18, 90, and 450 mA min−1, with a short measurement time of 60, 30, and 20 minutes. The resulting reproducibilities of Pb isotope ratios were comparable to those of previous techniques including the202Pb-205Pb double spike method and the204Pb-207Pb double spike method using an amplifier with a state-of-the-art 1013Ω resistor for collecting the204Pb signal. The absolute Pb isotope ratios for NIST 981 measured by our method were biased due to anomalous207Pb behavior occurring at the filament temperature of >1250 °C as well as the deterioration of Faraday cups. However, we confirmed that the accurate absolute Pb isotope ratios for an unknown sample can be obtained by normalizing the observed Pb isotope ratios to those of NIST 981 that are determined in the same analytical period and then multiplying the reference Pb isotope ratios of NIST 981. We measured the Pb isotope ratios of a standard rock material JB-3, of which the results were consistent with those reported by previous studies. We conclude that our method is suitable especially for the isotope analysis of sub-nanograms of Pb, and using a204Pb-207Pb double spike instead of a202Pb-205Pb double spike is beneficial for a number of laboratories due to the availability of the spikes. Furthermore, reduced measurement time compared to previous studies is helpful for measuring a large quantity of samples.

リンク情報
DOI
https://doi.org/10.1039/c6ja00455e
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