2021
DOI: 10.1016/j.jenvman.2021.112775
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Relevance of using the non-reactive geochemical signature in sediment core to estimate historical tributary contributions

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Cited by 5 publications
(2 citation statements)
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“…We can therefore assume a process of enhanced soil erosion in specific Isère River sub‐basins on Ni, Co and Cr element‐rich geological basements, leading to increasing concentrations of these TME over the past decade (2010s). However, only additional TME geochemical tracing methods, such as Pb, Cu and Zn isotopic fingerprinting techniques (Bird, 2011) or geochemical fingerprinting (Bégorre et al, 2021; Dabrin et al, 2021), could capture specific sources of TME in sediments. This heterogeneous pattern of the micropollutant yields of the Rhône River basin suggests that calculated micropollutants yields of the large river basins need to be considered with caution, in terms of the sources of the chemical fluxes.…”
Section: Discussionmentioning
confidence: 99%
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“…We can therefore assume a process of enhanced soil erosion in specific Isère River sub‐basins on Ni, Co and Cr element‐rich geological basements, leading to increasing concentrations of these TME over the past decade (2010s). However, only additional TME geochemical tracing methods, such as Pb, Cu and Zn isotopic fingerprinting techniques (Bird, 2011) or geochemical fingerprinting (Bégorre et al, 2021; Dabrin et al, 2021), could capture specific sources of TME in sediments. This heterogeneous pattern of the micropollutant yields of the Rhône River basin suggests that calculated micropollutants yields of the large river basins need to be considered with caution, in terms of the sources of the chemical fluxes.…”
Section: Discussionmentioning
confidence: 99%
“…We can therefore assume a process of enhanced soil erosion in specific Isère River sub-basins on Ni, Co and Cr element-rich geological basements, leading to increasing concentrations of these TME over the past decade (2010s). However, only additional TME geochemical tracing methods, such as Pb, Cu and Zn isotopic fingerprinting techniques (Bird, 2011) or geochemical fingerprinting (Bégorre et al, 2021;Dabrin et al, 2021) As a result, regarding TME, the lack of geochemical background data for each river basin is a significant barrier to considering TME yields as a consistent proxy for assessing river basin contamination. Indeed, as it stands, TME yields reflect a mixture comprising both the TME fraction coming from the local geological environment and TME fraction from the anthropogenic activity.…”
Section: Assessment Of the Relationship Between The Micropollutant Yi...mentioning
confidence: 99%