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• W4280494505 abstract "The Mg isotope system helps constrain a variety of geochemical processes in the hydrosphere, lithosphere and biosphere. DSM3 is commonly used as delta‐zero material for relative Mg isotopic measurements. In this study, we have characterised the Mg isotopic composition of a new pure Mg solution (Alfa‐Mg). This solution could potentially be used as a secondary delta‐zero reference material, or as an alternative primary reference material when DSM3 is depleted. The Alfa‐Mg solution has been checked for homogeneity and stability and is available free of charge upon request. The certified δ 26 / 24 Mg value relative to DSM3 of the Alfa‐Mg solution is −1.40‰, with an expanded ( k = 2) uncertainty of 0.05‰. We also characterised a range of existing Earth‐surface reference materials including soils, riverine sediments and plants. The δ 26/24 Mg values (relative to DSM‐3) of plant materials range between −1.06 ± 0.03‰ (2 s , n = 12) and −0.75 ± 0.03‰ (2 s , n = 12). The δ 26/24 Mg values of soil materials vary from −0.72 ± 0.11‰ (2 s , n = 12) to 0.17 ± 0.05‰ (2 s , n = 12). The δ 26/24 Mg values of riverine sediment materials range between −0.66 ± 0.01‰ (2 s , n = 12) and −0.17 ± 0.03‰ (2 s , n = 12). These data could serve as a reference for inter‐laboratory calibration and quality control, as well as for potential applications in geological and biological fields." @default.
• W4280494505 created "2022-05-22" @default.
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• W4280494505 date "2022-07-12" @default.
• W4280494505 modified "2023-10-11" @default.
• W4280494505 title "Characterisation of a New <scp>Delta‐Zero</scp> Natural Mg Solution <scp>Alfa‐Mg</scp> for Isotope Ratio Measurement and Mg Isotopic Values in Fourteen Matrix Reference Materials" @default.
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• W4280494505 doi "https://doi.org/10.1111/ggr.12430" @default.
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