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Aerosol source (biomass, traffic and coal emission) apportionment in Lithuania using stable carbon and radiocarbon analysis. | LitMetric

AI Article Synopsis

  • The study used stable carbon isotope ratios and radiocarbon data to identify sources of aerosol emissions in Lithuania, analyzing filter samples from urban and rural locations during different seasons.
  • It was found that the highest amount of contemporary carbon was in rural areas during warm periods, while fossil fuel emissions were greater from industrialized regions at all times.
  • Traffic emissions accounted for 15% and 25% of total emissions in rural and urban sites, respectively, with coal-derived particles significantly present during cold periods.

Article Abstract

In the present study, a combination of the stable carbon isotope ratio (C/C) with radiocarbon data (C) allowed us to perform the aerosol source apportionment. Filter samples of PM were collected during the warm and cold periods in rural and urban sites in Lithuania. The C/C ratio of total carbon (TC) was measured using the single stage accelerator mass spectrometer quantifying of fossil and non-fossil derived aerosol emissions. The δC value was measured using an elemental analyser interfaced with an isotope ratio mass spectrometer. We have found that the highest fraction of contemporary carbon (f = 0.82) was measured during a warm period in a rural location. A higher fraction of fossil fuel-derived carbon was observed for air masses transported from highly industrialized Western European regions during both seasons. Isotope mass balance calculations revealed that the traffic emissions composed 15 and 25 % in rural and urban sites, respectively, and did not change during either season. Input from coal-derived aerosol particles was estimated to be 15 % at an urban site during the cold period. The combination of the stable carbon isotope ratio with the radiocarbon data allowed us to distinguish coal, liquid fossil fuel combustion, and non-fossil derived aerosol particle emissions.

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Source
http://dx.doi.org/10.1080/10256016.2018.1509074DOI Listing

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