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- W2068677549 abstract "This paper describes the results of isotopic analyses of (i) hydrogen and oxygen in water (δ D and δ18O) and (ii) sulphur and oxygen in sulphates (δ34Ssulphate and δ18Osulphate) from atmospheric precipitation collected within a one-year period between 25 May 2004 and 25 May 2005 in Wrocław (SW Poland). The resulting equation of Local Meteoric Water Line for Wrocław is δ D=6.373×δ18O−0.047, (r 2=0.97, n=32). The δ34Ssulphate varies from 1.1 to 4.2‰ (with an average of 2.5‰), δ18Osulphate varies from 9.0 to 16.7‰ (with an average of 13.8‰) and δ18O varies from−0.8 to−16.3‰ (with an average of−8.2‰). The above results indicate two main sources of sulphates in Wrocław precipitation: (i) low-temperature secondary sulphates forming in situ in Wrocław from the atmospheric SO2 as well as precipitation water (heterogeneous and homogeneous pathways oxidation) and (ii) high-temperature primary sulphates forming in rapid high-temperature hydratation of SO in an immediate proximity of industrial chimneys. We hypothesise that the secondary low-temperature type of sulphates is probably formed from the local sulphur and oxygen reservoirs, whereas the primary high-temperature type is allochthonous and it is probably transported from industrial areas located outside of Wrocław." @default.
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- W2068677549 date "2008-06-01" @default.
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- W2068677549 title "Isotopic composition of sulphates from meteoric precipitation as an indicator of pollutant origin in Wrocław (SW Poland)†" @default.
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- W2068677549 doi "https://doi.org/10.1080/10256010802066307" @default.
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