Aerosols in Northern Morocco-2: Chemical Characterization and PMF Source Apportionment of Ambient PM<sub>2.5</sub>

oleh: Abdelfettah Benchrif, Mounia Tahri, Benjamin Guinot, El Mahjoub Chakir, Fatiha Zahry, Bouamar Bagdhad, Moussa Bounakhla, Hélène Cachier, Francesca Costabile

Format: Article
Diterbitkan: MDPI AG 2022-10-01

Deskripsi

Insufficient data on the chemical composition of PM<sub>2.5</sub> and its emission sources in the southwestern (SW) Mediterranean area has been identified. Ambient PM<sub>2.5</sub> samples were collected in an urban area of Tetouan city, northern Morocco. Chemical mass closure calculations and positive matrix factorization were performed for the comprehensive dataset of PM<sub>2.5</sub> chemical analyses. Mass closure improved when multipliers (1.2 and 0.23, respectively) were used for the conversion of organic carbon (OC) and calcium ion (Ca<sup>2+</sup>) into particulate organic matter (POM) and mineral dust masses, respectively. The mass closure model performed well in this SW Mediterranean region, with a significant correlation (r<sup>2</sup> = 0.97) obtained between gravimetrically measured and chemically determined PM<sub>2.5</sub> mass. The one-year average concentration of PM<sub>2.5</sub> was 17.96 μg/m<sup>3</sup>, and the major chemical components were POM (34%), secondary inorganic aerosol (SIA) (28%), and black carbon (18%), while unidentified mass was 4%. The mass concentration and most of the chemical components of PM<sub>2.5</sub> showed clear seasonal variations, with a summer-high and winter-low pattern for SIA, dust, and BC. In the winter months, POM was the dominant component. Source apportionment analysis revealed that PM<sub>2.5</sub> emission sources, regarding their typical tracers, were ammonium sulfate (SO<sub>4</sub><sup>2−</sup>, NH<sub>4</sub><sup>+</sup>, K<sup>+</sup>, NO<sub>3</sub><sup>−</sup>), road traffic and biomass burning emissions (OC, BC), fresh sea salt (Cl<sup>−</sup>, K<sup>+</sup>, NO<sub>3</sub><sup>−</sup>), aged sea salt (Mg<sup>2+</sup>, Na<sup>+</sup>, Ca<sup>2+</sup>), and oxalate-rich (oxalate, NO<sub>3</sub><sup>−</sup>) factors. Further, it is hoped that these findings help to improve the scientific understanding of SW Mediterranean aerosols.