Katarzyna Pawlak , Agata Błaziak , Bartłomiej Witkowski , Tomasz Gierczak , Rafał Szmigielski
{"title":"α-蒎烯和δ-3-蒈烯衍生SOA组分在水相OH自由基作用下形成萜烯酸及其动力学研究","authors":"Katarzyna Pawlak , Agata Błaziak , Bartłomiej Witkowski , Tomasz Gierczak , Rafał Szmigielski","doi":"10.1016/j.atmosenv.2025.121587","DOIUrl":null,"url":null,"abstract":"<div><div>Bimolecular reaction rate coefficients (k<sub>OH</sub>, L mol<sup>−1</sup>s<sup>−1</sup>) for the aqueous oxidation of pinic, caric, caronic, norpinic, and norpinonic acids by OH radicals were measured within the presented study. Furthermore, a quantitative analysis was performed for selected products formed in the studied OH reactions, including those known in the literature, SOA components of α-pinene and δ-3-carene. Values of k<sub>OH</sub> were measured for the neutral (pH = 2) and deprotonated (pH = 10) forms of the terpenoic acids under investigation in the temperature range between 288 and 308 K. The reactions of caronic and caric acids with OH radicals appear slightly faster (k<sub>OH</sub><sup>298K pH2</sup> = 3.3 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup> and k<sub>OH</sub><sup>298K pH2</sup> = 3.3 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>, respectively) than those of norpinic (k<sub>OH</sub><sup>298K pH2</sup> = 1.2 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>), norpinonic (k<sub>OH</sub><sup>298K pH2</sup> = 1.1 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>) and pinic acids (k<sub>OH</sub><sup>298K pH2</sup> = 2.1 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>). The calculated activation energies (E) fall in a 9–21 kJ mol<sup>−1</sup> range, explaining the very weak temperature dependence of the measured reaction rates. The calculated lifetimes decreased with increasing LWC (from 10<sup>−12</sup> m<sup>3</sup> m<sup>3</sup> in aerosol to 10<sup>−5</sup> m<sup>3</sup> m<sup>−3</sup> in storms), indicating that the acids undergo significant aqueous processing under realistic atmospheric conditions. The analysis of extremely low-volatility products allowed proposing reaction paths from earlier– to later–generation products (only carboxylic acid) of α-pinene. We measured that terebic acid can be formed through the aqueous phase OH reaction of norpinic acid, but also through terpenylic acid oxidation. Moreover, we found that the reaction of terpenylic acid + OH radicals is almost 10 times slower than the oxidation of pinic and pinonic acids. Therefore, observed in the atmosphere, terebic acid formation is mainly through direct oxidation of an early-generation oxidation product of α-pinene (pinic and pinonic acids) rather than from the secondary reaction of terpenylic acid.</div></div>","PeriodicalId":250,"journal":{"name":"Atmospheric Environment","volume":"362 ","pages":"Article 121587"},"PeriodicalIF":3.7000,"publicationDate":"2025-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Formation and kinetics of terpenoic acids from α-pinene and δ-3-carene-derived SOA components via aqueous-phase OH radicals\",\"authors\":\"Katarzyna Pawlak , Agata Błaziak , Bartłomiej Witkowski , Tomasz Gierczak , Rafał Szmigielski\",\"doi\":\"10.1016/j.atmosenv.2025.121587\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Bimolecular reaction rate coefficients (k<sub>OH</sub>, L mol<sup>−1</sup>s<sup>−1</sup>) for the aqueous oxidation of pinic, caric, caronic, norpinic, and norpinonic acids by OH radicals were measured within the presented study. Furthermore, a quantitative analysis was performed for selected products formed in the studied OH reactions, including those known in the literature, SOA components of α-pinene and δ-3-carene. Values of k<sub>OH</sub> were measured for the neutral (pH = 2) and deprotonated (pH = 10) forms of the terpenoic acids under investigation in the temperature range between 288 and 308 K. The reactions of caronic and caric acids with OH radicals appear slightly faster (k<sub>OH</sub><sup>298K pH2</sup> = 3.3 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup> and k<sub>OH</sub><sup>298K pH2</sup> = 3.3 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>, respectively) than those of norpinic (k<sub>OH</sub><sup>298K pH2</sup> = 1.2 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>), norpinonic (k<sub>OH</sub><sup>298K pH2</sup> = 1.1 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>) and pinic acids (k<sub>OH</sub><sup>298K pH2</sup> = 2.1 ± 0.1 × 10<sup>9</sup> L mol<sup>−1</sup>s<sup>−1</sup>). The calculated activation energies (E) fall in a 9–21 kJ mol<sup>−1</sup> range, explaining the very weak temperature dependence of the measured reaction rates. The calculated lifetimes decreased with increasing LWC (from 10<sup>−12</sup> m<sup>3</sup> m<sup>3</sup> in aerosol to 10<sup>−5</sup> m<sup>3</sup> m<sup>−3</sup> in storms), indicating that the acids undergo significant aqueous processing under realistic atmospheric conditions. The analysis of extremely low-volatility products allowed proposing reaction paths from earlier– to later–generation products (only carboxylic acid) of α-pinene. We measured that terebic acid can be formed through the aqueous phase OH reaction of norpinic acid, but also through terpenylic acid oxidation. Moreover, we found that the reaction of terpenylic acid + OH radicals is almost 10 times slower than the oxidation of pinic and pinonic acids. Therefore, observed in the atmosphere, terebic acid formation is mainly through direct oxidation of an early-generation oxidation product of α-pinene (pinic and pinonic acids) rather than from the secondary reaction of terpenylic acid.</div></div>\",\"PeriodicalId\":250,\"journal\":{\"name\":\"Atmospheric Environment\",\"volume\":\"362 \",\"pages\":\"Article 121587\"},\"PeriodicalIF\":3.7000,\"publicationDate\":\"2025-10-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Atmospheric Environment\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S135223102500562X\",\"RegionNum\":2,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atmospheric Environment","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S135223102500562X","RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Formation and kinetics of terpenoic acids from α-pinene and δ-3-carene-derived SOA components via aqueous-phase OH radicals
Bimolecular reaction rate coefficients (kOH, L mol−1s−1) for the aqueous oxidation of pinic, caric, caronic, norpinic, and norpinonic acids by OH radicals were measured within the presented study. Furthermore, a quantitative analysis was performed for selected products formed in the studied OH reactions, including those known in the literature, SOA components of α-pinene and δ-3-carene. Values of kOH were measured for the neutral (pH = 2) and deprotonated (pH = 10) forms of the terpenoic acids under investigation in the temperature range between 288 and 308 K. The reactions of caronic and caric acids with OH radicals appear slightly faster (kOH298K pH2 = 3.3 ± 0.1 × 109 L mol−1s−1 and kOH298K pH2 = 3.3 ± 0.1 × 109 L mol−1s−1, respectively) than those of norpinic (kOH298K pH2 = 1.2 ± 0.1 × 109 L mol−1s−1), norpinonic (kOH298K pH2 = 1.1 ± 0.1 × 109 L mol−1s−1) and pinic acids (kOH298K pH2 = 2.1 ± 0.1 × 109 L mol−1s−1). The calculated activation energies (E) fall in a 9–21 kJ mol−1 range, explaining the very weak temperature dependence of the measured reaction rates. The calculated lifetimes decreased with increasing LWC (from 10−12 m3 m3 in aerosol to 10−5 m3 m−3 in storms), indicating that the acids undergo significant aqueous processing under realistic atmospheric conditions. The analysis of extremely low-volatility products allowed proposing reaction paths from earlier– to later–generation products (only carboxylic acid) of α-pinene. We measured that terebic acid can be formed through the aqueous phase OH reaction of norpinic acid, but also through terpenylic acid oxidation. Moreover, we found that the reaction of terpenylic acid + OH radicals is almost 10 times slower than the oxidation of pinic and pinonic acids. Therefore, observed in the atmosphere, terebic acid formation is mainly through direct oxidation of an early-generation oxidation product of α-pinene (pinic and pinonic acids) rather than from the secondary reaction of terpenylic acid.
期刊介绍:
Atmospheric Environment has an open access mirror journal Atmospheric Environment: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review.
Atmospheric Environment is the international journal for scientists in different disciplines related to atmospheric composition and its impacts. The journal publishes scientific articles with atmospheric relevance of emissions and depositions of gaseous and particulate compounds, chemical processes and physical effects in the atmosphere, as well as impacts of the changing atmospheric composition on human health, air quality, climate change, and ecosystems.