Influence of sulfur-bearing polyatomic species on high precision measurements of Cu isotopic composition
An increased interest in high precision Cu isotope ratio measurements using multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) has developed recently for various natural geologic systems and environmental applications, these typically contain high concentrations of sulfur, part...
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Veröffentlicht in: | Chemical geology 2010-04, Vol.272 (1), p.49-54 |
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Zusammenfassung: | An increased interest in high precision Cu isotope ratio measurements using multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) has developed recently for various natural geologic systems and environmental applications, these typically contain high concentrations of sulfur, particularly in the form of sulfate (SO
4
2−) and sulfide (S). For example, Cu, Fe, and Zn concentrations in acid mine drainage (AMD) can range from 100
µg/L to greater than 50
mg/L with sulfur species concentrations reaching greater than 1000
mg/L. Routine separation of Cu, Fe and Zn from AMD, Cu–sulfide minerals and other geological matrices usually incorporates single anion exchange resin column chromatography for metal separation. During chromatographic separation, variable breakthrough of SO
4
2− during anion exchange resin column chromatography into the Cu fractions was observed as a function of the initial sulfur to Cu ratio, column properties, and the sample matrix. SO
4
2− present in the Cu fraction can form a polyatomic
32S–
14N–
16O–
1H species causing a direct mass interference with
63Cu and producing artificially light
δ
65Cu values. Here we report the extent of the mass interference caused by SO
4
2− breakthrough when measuring
δ
65Cu on natural samples and NIST SRM 976 Cu isotope spiked with SO
4
2− after both single anion column chromatography and double anion column chromatography. A set of five 100
µg/L Cu SRM 976 samples spiked with 500
mg/L SO
4
2− resulted in an average
δ
65Cu of −
3.50‰
±
5.42‰ following single anion column separation with variable SO
4
2− breakthrough but an average concentration of 770
µg/L. Following double anion column separation, the average SO
4
2−concentration of 13
µg/L resulted in better precision and accuracy for the measured
δ
65Cu value of 0.01‰
±
0.02‰ relative to the expected 0‰ for SRM 976. We conclude that attention to SO
4
2− breakthrough on sulfur-rich samples is necessary for accurate and precise measurements of
δ
65Cu and may require the use of a double ion exchange column procedure. |
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ISSN: | 0009-2541 1872-6836 |
DOI: | 10.1016/j.chemgeo.2010.02.003 |