LEAD ISOTOPIC RATIO DETERMINATION IN CAVE SEDIMENTS USING TRIPLE-QUADRUPOLE INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRY

Authors

  • Anamaria Iulia TÖRÖK INCDO-INOE2000, Research Institute for Analytical Instrumentation, 67 Donath, RO-400293, Cluj-Napoca, Romania. https://orcid.org/0000-0003-2123-1871
  • Claudiu TĂNĂSELIA INCDO-INOE2000, Research Institute for Analytical Instrumentation, 67 Donath, RO-400293, Cluj-Napoca, Romania. *Corresponding author: claudiu.tanaselia@icia.ro https://orcid.org/0000-0001-8931-787X
  • Ana MOLDOVAN INCDO-INOE2000, Research Institute for Analytical Instrumentation, 67 Donath, RO-400293, Cluj-Napoca, Romania; Technical University, Faculty of Materials and Environmental Engineering, 103-105 Muncii Boulevard, 400641 Cluj-Napoca, Romania. https://orcid.org/0000-0001-8704-6121
  • Bogdan ANGYUS INCDO-INOE2000, Research Institute for Analytical Instrumentation, 67 Donath, RO-400293, Cluj-Napoca, Romania; Babes-Bolyai University, Faculty of Chemistry and Chemical Engineering, 11 Arany Janos, 400028 Cluj-Napoca, Romania. https://orcid.org/0000-0001-8073-6760
  • Erika Andrea LEVEI INCDO-INOE2000, Research Institute for Analytical Instrumentation, 67 Donath, RO-400293, Cluj-Napoca, Romania. https://orcid.org/0000-0002-0145-0287
  • Cecilia ROMAN INCDO-INOE2000, Research Institute for Analytical Instrumentation, 67 Donath, RO-400293, Cluj-Napoca, Romania. https://orcid.org/0000-0002-7838-1283

DOI:

https://doi.org/10.24193/subbchem.2021.4.02

Keywords:

ICP-MS, Pb isotopic ratio, lead, cave sediments, triple-quadrupole.

Abstract

Lead isotopic ratio determination is significantly affected by the isobaric interference of mercury (204Hg), thus many studies lack 204Pb/206Pb values. Removal of 204Hg from sample is resource consuming, while mathematical correction can be employed if the Hg isotope ratio in the sample is known. Triple quadrupole inductively coupled plasma mass spectrometry (TQ-ICP-MS) offers a mechanism for removing the 204Hg, by pressurizing the reaction cell with ammonia, that reacts with 204Hg positively charged ions rendering them neutral, thus filtering them out and removing them from the ion beam. The Pb isotope ratio determination can be used as “fingerprint” to identify the sources of contamination and environmental pollution. The method developed based on this mechanism was used for Pb isotopic ratio determination in cave sediment samples. Relative standard deviation of this method was between 0.36% - 0.59%.

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Published

2021-12-30

How to Cite

TÖRÖK, A. I., TĂNĂSELIA, C., MOLDOVAN, A., ANGYUS, B., LEVEI, E. A., & ROMAN, C. (2021). LEAD ISOTOPIC RATIO DETERMINATION IN CAVE SEDIMENTS USING TRIPLE-QUADRUPOLE INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRY. Studia Universitatis Babeș-Bolyai Chemia, 66(4), 23–31. https://doi.org/10.24193/subbchem.2021.4.02

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