Afnan Al-Hunaiti , Zaid Bakri , Xinyang Li , Lian Duan , Asal Al-Abdallat , Andres Alastuey , Mar Viana , Sharif Arar , Tuukka Petäjä , Tareq Hussein
{"title":"Characterization of water-soluble inorganic ions and carbonaceous aerosols in the urban atmosphere in Amman, Jordan","authors":"Afnan Al-Hunaiti , Zaid Bakri , Xinyang Li , Lian Duan , Asal Al-Abdallat , Andres Alastuey , Mar Viana , Sharif Arar , Tuukka Petäjä , Tareq Hussein","doi":"10.1016/j.pce.2024.103783","DOIUrl":null,"url":null,"abstract":"<div><div>The urban particulate matter (PM) carbonaceous and water-soluble ions were investigated in Amman, Jordan during May 2018–March 2019. The PM<sub>2.5</sub> total carbon (TC) annual mean was 7.6 ± 3.6 μg/m<sup>3</sup> (organic carbon (OC) 5.9 ± 2.8 μg/m<sup>3</sup> and elemental carbon (EC) 1.7 ± 1.1 μg/m<sup>3</sup>), which was about 16.3% of the PM<sub>2.5</sub>. The PM<sub>10</sub> TC annual mean was 8.4 ± 3.9 μg/m<sup>3</sup> (OC 6.5 ± 3.1 μg/m<sup>3</sup> and elemental carbon (EC) 1.9 ± 1.1 μg/m<sup>3</sup>), about 13.3% of the PM<sub>10</sub>. The PM<sub>2.5</sub> total water-soluble ions annual mean was 7.9 ± 1.9 μg/m<sup>3</sup> (about 16.9%), and that of the PM<sub>10</sub> was 10.1 ± 2.8 μg/m<sup>3</sup> (about 16.0%). The minor ions (F<sup>−</sup>, NO<sub>2</sub><sup>−</sup>, Br<sup>−</sup>, and PO<sub>4</sub><sup>3−</sup>) constituted less than 1% in the PM fractions. The significant fraction was for SO<sub>4</sub><sup>2−</sup> (PM<sub>2.5</sub> 4.7 ± 1.6 μg/m<sup>3</sup> (10.0%) and PM<sub>10</sub> 5.3 ± 1.9 μg/m<sup>3</sup> (8.3%)). The NH<sub>4</sub><sup>+</sup> had higher amounts of PM<sub>2.5</sub> (1.3 ± 0.6 μg/m3; 2.7%) than that PM<sub>10</sub> (0.9 ± 0.4 μg/m<sup>3</sup>; 1.4%). During sand and dust storm (SDS) events, TC, Cl<sup>−</sup>, and NO<sub>3</sub><sup>−</sup> were doubled in PM, SO<sub>4</sub><sup>2−</sup> did not increase significantly, and NH<sub>4</sub><sup>+</sup> slightly decreased. Regression analysis revealed: (1) carbonaceous aerosols come equally from primary and secondary sources, (2) about 50% of the OC came from non-combustion sources, (3) traffic emissions dominate the PM, (4) agricultural sources have a negligible effect, (5) SO<sub>4</sub><sup>2−</sup> is completely neutralized by NH<sub>4</sub><sup>+</sup> in the PM<sub>2.5</sub> but there could be additional reactions involved in the PM<sub>10</sub>, and (6) (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub>, was the major species formed by SO<sub>4</sub><sup>2−</sup>and NH<sub>4</sub><sup>+</sup> instead of NH<sub>4</sub>HSO<sub>4</sub>. It is recommended to perform long-term sampling and chemical speciation for the urban atmosphere in Jordan.</div></div>","PeriodicalId":54616,"journal":{"name":"Physics and Chemistry of the Earth","volume":"136 ","pages":"Article 103783"},"PeriodicalIF":3.0000,"publicationDate":"2024-10-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics and Chemistry of the Earth","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1474706524002419","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
The urban particulate matter (PM) carbonaceous and water-soluble ions were investigated in Amman, Jordan during May 2018–March 2019. The PM2.5 total carbon (TC) annual mean was 7.6 ± 3.6 μg/m3 (organic carbon (OC) 5.9 ± 2.8 μg/m3 and elemental carbon (EC) 1.7 ± 1.1 μg/m3), which was about 16.3% of the PM2.5. The PM10 TC annual mean was 8.4 ± 3.9 μg/m3 (OC 6.5 ± 3.1 μg/m3 and elemental carbon (EC) 1.9 ± 1.1 μg/m3), about 13.3% of the PM10. The PM2.5 total water-soluble ions annual mean was 7.9 ± 1.9 μg/m3 (about 16.9%), and that of the PM10 was 10.1 ± 2.8 μg/m3 (about 16.0%). The minor ions (F−, NO2−, Br−, and PO43−) constituted less than 1% in the PM fractions. The significant fraction was for SO42− (PM2.5 4.7 ± 1.6 μg/m3 (10.0%) and PM10 5.3 ± 1.9 μg/m3 (8.3%)). The NH4+ had higher amounts of PM2.5 (1.3 ± 0.6 μg/m3; 2.7%) than that PM10 (0.9 ± 0.4 μg/m3; 1.4%). During sand and dust storm (SDS) events, TC, Cl−, and NO3− were doubled in PM, SO42− did not increase significantly, and NH4+ slightly decreased. Regression analysis revealed: (1) carbonaceous aerosols come equally from primary and secondary sources, (2) about 50% of the OC came from non-combustion sources, (3) traffic emissions dominate the PM, (4) agricultural sources have a negligible effect, (5) SO42− is completely neutralized by NH4+ in the PM2.5 but there could be additional reactions involved in the PM10, and (6) (NH4)2SO4, was the major species formed by SO42−and NH4+ instead of NH4HSO4. It is recommended to perform long-term sampling and chemical speciation for the urban atmosphere in Jordan.
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