Source identification of PM2.5 carbonaceous aerosol using combined carbon fraction, radiocarbon and stable carbon isotope analyses in Debrecen, Hungary

In this study, PM2.5 aerosol samples collected continuously in Debrecen, Hungary from December 2011 to July 2014 were processed and analysed. Mass concentration and ratios of PM2.5 aerosol, organic and elemental carbon fractions, in addition, radio and stable carbon isotopes were evaluated together to obtain a better sight into the possible local and regional sources. For the studied period, the mean mass concentration of PM2.5 aerosol and the constituting total, organic and elemental carbon were 23.6, 5.8, 5.0 and 0.8 mu g m(-3), respectively. In all cases, the mean for the heating periods were on average 2-3 times that of the vegetation (i.e. heating-free) periods. The relatively high mean secondary organic carbon concentration of 4.1 mu g m(-3) and OC/EC ratio of 6.9 suggested the dominance of combustion processes in winter and, based on the higher contemporary carbon fraction of 0.77, wood fuels prevailed over coal or oil. The average delta C-13 of the tested wood fuels implies that combustion of black locust, oak and beech was a significant factor in forming the mean delta C-13 of PM2.5 of -25.6% during the heating months. The mean delta C-13 of -26.7% in summer was more influenced by emissions from transportation and the surrounding vegetation. In addition, using coupled backward trajectory modeling (HYSPLIT) and visualization of open fire events (FIRMS), we presume that the conspicuously enriched delta C-13 values of PM2.5 collected in October of the observation years were probably caused by long-range transport of particles derived from agricultural combustion of C-4 plants close to the southern and eastern Hungarian borders. (C) 2021 The Authors. Published by Elsevier B.V.

Automated summary

This study analyzed PM2.5 aerosol samples collected in Debrecen, Hungary from 2011 to 2014, finding that combustion processes dominated in winter with wood fuels prevailing. Additionally, enriched ΔC-13 values in October were likely caused by long-range transport of particles from agricultural combustion of C-4 plants.