Chemical Procedures for Rhenium Extraction from Geological Samples: Optimising the Anion Resin Bead Clean‐up Step

Rhenium–osmium geochronometry for samples with low Re and complex matrices requires improved Re extraction methods. Here, we investigate plausible controls on efficiency and efficacy of Re extraction during our anion resin bead purification. Four different protocols are compared, each isolating a si...

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Bibliographic Details
Published in:Geostandards and geoanalytical research 2020-06, Vol.44 (2), p.231-242
Main Authors: Yang, Gang, Zimmerman, Aaron, Hurtig, Nicole C., Georgiev, Svetoslav V., Goswami, Vineet, Hannah, Judith L., Stein, Holly J.
Format: Article
Language:English
Subjects:
anion resin bead
Anions
Chemical recovery
Duration
emission efficiency
Emission measurements
Geochronometry
Geological samples
ICP‐MS
Ions
Isotopes
Mass spectrometry
Mass spectroscopy
Nitric acid
Nitric acids
N‐TIMS
Osmium
Protocol
Re chemistry
Recovery
Rhenium
Water purification
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Summary:Rhenium–osmium geochronometry for samples with low Re and complex matrices requires improved Re extraction methods. Here, we investigate plausible controls on efficiency and efficacy of Re extraction during our anion resin bead purification. Four different protocols are compared, each isolating a single variable to test. Rhenium concentrations for solutions at each step of each protocol document differences in chemical recovery/yield. The negative‐thermal ionisation mass spectrometry (N‐TIMS) signal intensity serves as a proxy for Re yield and purity. These data document correlations between the N‐TIMS signal intensity and (a) the duration of anion resin bead conditioning prior to loading with Re‐bearing solution, and (b) both duration and strength of nitric acid used during rinsing of the Re‐loaded anion resin bead. The optimal protocol improved Re signal intensity around fourteen times compared with our current Re extraction protocol, an aggregate of 2.4 times improvement in chemical recovery (yield) and 5.8 times improvement in emission efficiency (purity). Repeated N‐TIMS isotopic measurements on our in‐house Re standard solution (1407) verify that our optimal protocol‐3 does not fractionate Re isotopes. The improved anion resin bead method considerably lowers the Re detection limit and allows Re‐Os isotopic analysis of picogram‐level Re hosted in geological samples with complex matrices. Key Points We investigate plausible controls on efficiency and efficacy of Re extraction during anion resin bead purification We identify an optimal protocol which increases Re signal intensity 14x compared with our current Re extraction protocol. Critically, no mass fractionation between Re isotopes was observed.
ISSN:1639-4488
1751-908X
DOI:10.1111/ggr.12318