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Lead isotopic ratio determination in cave sediments using triple-quadrupole inductively coupled plasma mass spectrometry
2021
Studia Universitatis Babe?-Bolyai Chemia
Lead isotopic ratio determination is significantly affected by the isobaric interference of mercury ( 204 Hg), thus many studies lack 204 Pb/ 206 Pb values. Removal of 204 Hg 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 204 Hg, by pressurizing the reaction cell with ammonia, that reacts with 204 Hg
doi:10.24193/subbchem.2021.4.02
fatcat:4q6xzcgu3zaq7jim5mdtsximby