z-logo
Premium
Copper Isotopic Analysis in Geological and Biological Reference Materials by MC‐ICP‐MS
Author(s) -
Sullivan Kaj,
LaytonMatthews Daniel,
Leybourne Matthew,
Kidder James,
Mester Zoltán,
Yang Lu
Publication year - 2020
Publication title -
geostandards and geoanalytical research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.037
H-Index - 73
eISSN - 1751-908X
pISSN - 1639-4488
DOI - 10.1111/ggr.12315
Subject(s) - hydrosphere , sediment , copper , basalt , environmental chemistry , biosphere , oil shale , mineralogy , geology , geochemistry , environmental science , chemistry , paleontology , ecology , organic chemistry , biology
The characterisation of relative copper isotope amount ratios (δ 65 Cu) helps constrain a variety of geochemical processes occurring in the geosphere, biosphere and hydrosphere. The accurate and precise determination of δ 65 Cu in matrix reference materials is crucial in the effort to validate measurement methods. With the goal of expanding the number and variety of available geological and biological materials, we have characterised the δ 65 Cu values of ten reference materials by MC‐ICP‐MS using C‐SSBIN model for mass bias correction. SGR‐1b (Green River shale), DOLT‐5 (dogfish liver), DORM‐4 (fish protein), TORT‐3 (lobster hepatopancreas), MESS‐4 (marine sediment) and PACS‐3 (marine sediment) have for the first time been characterised for δ 65 Cu. Additionally, four reference materials (with published δ 65 Cu values) have been characterised: BHVO‐1 (Hawaiian basalt), BIR‐1 (Icelandic basalt), W‐2a (diabase) and Seronorm™ Trace Elements Serum L‐1 (human serum). The reference materials measured in this study possess complex and varied matrices with copper mass fractions ranging from 1.2 µg g −1 to 497 µg g −1 and δ 65 Cu values ranging from −0.20‰ to 0.52‰ with a mean expanded uncertainty of ± 0.07‰ ( U , k  = 2), covering much of the natural copper isotope variability observed in the environment.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here