Abstract
Natural variation in the isotopic composition of Sb in stibnites (Sb ores) was explored using multi-collector ICP-mass spectrometry (MC-ICP-MS). A method for isolating Sb (after acid digestion) without introducing artificial mass fractionation was developed, based on the use of a combination of cation exchange chromatography using Dowex AG50-X8 resin and anion exchange chromatography using Amberlite IRA 743 resin. For pure stibnites (Sb2S3), Sb isolation is not strictly required as at a 2 : 3 Sb : S molar ratio, it was demonstrated that the concomitant S does not affect the 123Sb/121Sb isotope ratio result. However, the method can be deployed for other Sb ore types with a lower Sb : S ratio and for samples with lower purity. Indium was used as an internal standard for correction of the instrument-induced mass discrimination occurring in the MC-ICP-MS instrument. The 123Sb/121Sb ratio could be measured with 0.002% repeatability (internal precision), while for the samples the 123e values were characterized by an uncertainty of 1 e unit. The isotopic composition of the selected materials (stibnites from various regions of the world) shows a variation spanning 10 e units (or 0.1%). The method developed shows potential to be used in provenance determination studies of ancient glass.
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