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Polycyclic Aromatic Hydrocarbons in Soils from European High Mountain Areas
Authors:Roberto Quiroz  Joan O Grimalt  Pilar Fernandez  Lluis Camarero  Jordi Catalan  Evzen Stuchlik  Hansjoerg Thies  Ulrike Nickus
Institution:1. Department of Environmental Chemistry, Institute of Environmental Assessment and Water Research (ID?A-CSIC), Jordi Girona 18-26, 08034, Barcelona, Catalonia, Spain
2. Limnology Unit (CSIC-UB), Centre for Advanced Studies of Blanes (CEAB-CSIC), Acc??s Cala St. Francesc, 14, 17300, Blanes, Catalonia, Spain
3. Department of Hydrology, Charles University, Vinicn?? 7, 12044, Prague, Czech Republic
4. Institute of Ecology, University of Innsbruck, Technikerstrasse 25, 6020, Innsbruck, Austria
5. Institute of Meteorology and Geophysics, University of Innsbruck, Innrain 52, 6020, Innsbruck, Austria
Abstract:Polycyclic aromatic hydrocarbons (PAHs) were analyzed in 70 soils distributed in mountain areas such as Montseny (300?C1,700 m), Pyrenees (1,500?C2,900 m), Alps (1,100?C2,500 m), and Tatras (1,400?C1,960 m). Average total PAH concentrations, excluding retene and perylene, were about 400 ng/g in the Pyrenees and 1,300?C1,600 ng/g in the other mountain ranges. No correlations between PAH concentrations and total organic carbon were observed. Retene was the major PAH in the Pyrenean soils of lower altitude. No altitudinal dependence was found between soil PAH concentrations and elevation for the whole dataset. However, in the Tatra soils a statistically significant correlation with altitude was observed involving higher concentrations at higher altitude. This correlation was due to the statistically significant altitudinal dependence of the more volatile PAHs. Another observed altitudinal trend concerned the benza]anthracene/(benza]anthracene + chrysene + triphenylene) and the benzoa]pyrene/(benzoa]pyrene + benzoe]pyrene) ratios that exhibited a decrease in the more chemically labile compounds, benza]anthracene and benzoa]pyrene, respectively, in the soils located at higher altitude. This observation is consistent with the expected higher photooxidation at higher mountain altitude.
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