Identifying the origins of local atmospheric deposition in the steel industry basin of Luxembourg using the chemical and isotopic composition of the lichen Xanthoria parietina

International audience ; Trace metal atmospheric contamination was assessed in one of the oldest European industrial sites of steel production situated in the southern part of the Grand-Duchy of Luxembourg. Using elemental ratios as well as Pb, Sr, and Nd isotopic compositions as tracers, we found preliminary results concerning the trace metal enrichment and the chemical/isotopic signatures of the most important emission sources using the lichen Xanthoria parietina sampled at 15 sites along a SW-NE transect. The concentrations of these elements decreased with increasing distance from the histo... Mehr ...

Verfasser: Hissler, C.
Stille, P.
Krein, A.
Lahd Geagea, M.
Perrone, T.
Probst, J.L.
Hoffman, L.
Dokumenttyp: Artikel
Erscheinungsdatum: 2008
Verlag/Hrsg.: HAL CCSD
Schlagwörter: Air contamination / Lichen monotoring / Soils / Isotopic signatures / Lead / Strontium / Neodymium / Rare Earth Elements (REE) / Luxembourg / [SDV.EE]Life Sciences [q-bio]/Ecology / environment
Sprache: Englisch
Permalink: https://search.fid-benelux.de/Record/base-29521135
Datenquelle: BASE; Originalkatalog
Powered By: BASE
Link(s) : https://hal.science/halsde-00335625

International audience ; Trace metal atmospheric contamination was assessed in one of the oldest European industrial sites of steel production situated in the southern part of the Grand-Duchy of Luxembourg. Using elemental ratios as well as Pb, Sr, and Nd isotopic compositions as tracers, we found preliminary results concerning the trace metal enrichment and the chemical/isotopic signatures of the most important emission sources using the lichen Xanthoria parietina sampled at 15 sites along a SW-NE transect. The concentrations of these elements decreased with increasing distance from the historical and actual steel-work areas. The combination of the different tracers (major elements, Rare Earth Element ratios, Pb, Sr and Nd isotopes) enabled us to distinguish between three principal sources: the historical steel production (old tailings corresponding to blast-furnace residues), the present steel production (industrial sites with arc electric furnace units) and the regional background (baseline) components. Other anthropogenic sources including a waste incinerator and major roads had only weak impacts on lichen chemistry and isotopic ratios. The correlation between the Sr and Nd isotope ratios indicated that the Sr–Nd isotope systems represented useful tools to trace atmospheric emissions of factories using scrap metal for steel production.