Stable isotope tracing of Ni and Cu pollution in North-East Norway: Potentials and drawbacks

The use of Ni and Cu isotopes for tracing contamination sources in the environment remains a challenging task due to the limited information about the influence of various biogeochemical processes influencing stable isotope fractionation. This work focuses on a relatively simple system in north-east Norway with two possible endmembers (smelter-bedrock) and various environmental samples (snow, soil, lichens, PM₁₀). In general, the whole area is enriched in heavy Ni and Cu isotopes highlighting the impact of the smelting activity. However, the environmental samples exhibit a large range of δ⁶⁰Ni (-0.01 ± 0.03‰ to 1.71 ± 0.02‰) and δ⁶⁵Cu (-0.06 ± 0.06‰ to -3.94 ± 0.3‰) values which exceeds the range of δ⁶⁰Ni and δ⁶⁵Cu values determined in the smelter, i.e. in feeding material and slag (δ⁶⁰Ni from 0.56 ± 0.06‰ to 1.00 ± 0.06‰ and δ⁶⁵Cu from -1.67 ± 0.04‰ to -1.68 ± 0.15‰). The shift toward heavier Ni and Cu δ values was the most significant in organic rich topsoil samples in the case of Ni (δ⁶⁰Ni up to 1.71 ± 0.02‰) and in lichens and snow in the case of Cu (δ⁶⁵Cu up to -0.06 ± 0.06‰ and -0.24 ± 0.04‰, respectively). These data suggest an important biological and biochemical fractionation (microorganisms and/or metal uptake by higher plants, organo-complexation etc.) of Ni and Cu isotopes, which should be quantified separately for each process and taken into account when using the stable isotopes for tracing contamination in the environment.