Characterization of water-soluble organic carbon absorption at an urban background site in the south-eastern Iberian Peninsula

Measurements of absorption coefficients (σap,λ) and carbonaceous components (OC, EC, WSOC and levoglucosan) in PM1 were conducted at an urban background site in southeastern Spain throughout 2021. The main goal of this research was to determine the contribution from different sources to WSOC light a...

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Veröffentlicht in:Atmospheric environment (1994) 2024-05, Vol.324, p.120435, Article 120435
Hauptverfasser: López-Caravaca, A., Crespo, J., Galindo, N., Yubero, E., Clemente, A., Castañer, R., Nicolás, J.F.
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container_end_page
container_issue
container_start_page 120435
container_title Atmospheric environment (1994)
container_volume 324
creator López-Caravaca, A.
Crespo, J.
Galindo, N.
Yubero, E.
Clemente, A.
Castañer, R.
Nicolás, J.F.
description Measurements of absorption coefficients (σap,λ) and carbonaceous components (OC, EC, WSOC and levoglucosan) in PM1 were conducted at an urban background site in southeastern Spain throughout 2021. The main goal of this research was to determine the contribution from different sources to WSOC light absorption (σWSOC). For this, σBrC,λ values were previously obtained. The mean contribution of BrC to total aerosol absorption was ∼29% at 370 nm, revealing a significant influence of BrC to light absorption in the study area. Assuming that BrC light absorption was from WSOC and WIOC, a multilinear regression (MLR) model was used to estimate σWSOC and σWIOC. Average values (mean ± SD) were very similar for both components: σWSOC,370 = 1.6 (±0.7) Mm−1 and σWIOC,370 = 1.9 (±0.7) Mm−1. Finally, the PMF technique coupled with MLR analysis was used to identify the sources of WSOC light absorption and estimate their contribution. Our findings point to biomass burning as the dominant source of σWSOC during the cold season, with a contribution of ∼37%. The Mineral Dust and Secondary Nitrate sources, that were not included in the model due to their low contribution to WSOC mass concentrations, accounted for a significant percentage of σWSOC during this period. Secondary organic aerosol was the major source during the warm season (∼56%), followed by traffic emissions (∼30%). •Sources of WSOC absorption was analysed at an urban background site in the southeast of the Iberian Peninsula.•BrC accounted for 29% of the total aerosol absorption at 370 nm, with similar contributions from WSOC and WIOC.•Marked seasonal variation of WSOC absorption, with higher levels during the cold season when BB emissions are highest.
doi_str_mv 10.1016/j.atmosenv.2024.120435
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The main goal of this research was to determine the contribution from different sources to WSOC light absorption (σWSOC). For this, σBrC,λ values were previously obtained. The mean contribution of BrC to total aerosol absorption was ∼29% at 370 nm, revealing a significant influence of BrC to light absorption in the study area. Assuming that BrC light absorption was from WSOC and WIOC, a multilinear regression (MLR) model was used to estimate σWSOC and σWIOC. Average values (mean ± SD) were very similar for both components: σWSOC,370 = 1.6 (±0.7) Mm−1 and σWIOC,370 = 1.9 (±0.7) Mm−1. Finally, the PMF technique coupled with MLR analysis was used to identify the sources of WSOC light absorption and estimate their contribution. Our findings point to biomass burning as the dominant source of σWSOC during the cold season, with a contribution of ∼37%. The Mineral Dust and Secondary Nitrate sources, that were not included in the model due to their low contribution to WSOC mass concentrations, accounted for a significant percentage of σWSOC during this period. 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subjects absorption
aerosols
biomass
BrC
Carbonaceous aerosol
cold season
dust
environment
Iberian Peninsula
MLR
nitrates
organic carbon
Sources
Spain
traffic
warm season
water solubility
WSOC absorption
title Characterization of water-soluble organic carbon absorption at an urban background site in the south-eastern Iberian Peninsula
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