Daniele Scheres Firak, Thomas Schaefer, Celine Kula, Nazanin Taherkhani and Hartmut Herrmann*,
{"title":"硫酸盐存在下Fenton反应中的离子强度效应及其对水颗粒相的影响","authors":"Daniele Scheres Firak, Thomas Schaefer, Celine Kula, Nazanin Taherkhani and Hartmut Herrmann*, ","doi":"10.1021/acsearthspacechem.4c0036210.1021/acsearthspacechem.4c00362","DOIUrl":null,"url":null,"abstract":"<p >Fenton chemistry [Fe(II) + H<sub>2</sub>O<sub>2</sub>] is a critical source of hydroxyl radicals (<sup>•</sup>OH) in deliquescent aerosols, yet its efficiency is significantly modulated by the high ionic strength (<i>I</i>) of these systems. This study investigates the influence of elevated sulfate concentrations on Fenton reactions under aerosol-relevant conditions. The isolated effect of ionic strength was first studied by using NaClO<sub>4</sub> as a model electrolyte. Results reveal that the Fenton reaction rate constant decreases sharply to 16 ± 1 M<sup>–1</sup> s<sup>–1</sup> until <i>I</i> = 2 M, increasing at higher <i>I</i> values. Fe(II) oxidation by dissolved O<sub>2</sub> increased to 282 ± 46 M<sup>–1</sup> s<sup>–1</sup> at <i>I</i> = 8 M, although dissolved O<sub>2</sub> concentrations are expected to decrease due to salting-out effects on oxygen. In Na<sub>2</sub>SO<sub>4</sub> solutions, Fe speciation shifts to FeSO<sub>4</sub>, resulting in enhanced rate constants, reaching 239 ± 21 M<sup>–1</sup> s<sup>–1</sup> at <i>I</i> = 2.7 M. Interestingly, Fe(II) oxidation by O<sub>2</sub> is negligible in Na<sub>2</sub>SO<sub>4</sub> solutions. The final OH yield remained unchanged in FeSO<sub>4</sub> solutions and decreased markedly in NaClO<sub>4</sub> solutions. Arrhenius expressions were derived for the Fenton reaction in 3.6 M NaClO<sub>4</sub> <i>k</i>(<i>T</i>) = (8.7 ± 0.8) × 10<sup>7</sup> × exp[(−4276 ± 520 K)/<i>T</i>] and the reaction in the presence of 1.2 M Na<sub>2</sub>SO<sub>4</sub>, <i>k</i>(<i>T</i>) = (7.5 ± 0.2) × 10<sup>9</sup> × exp[(−5153 ± 310 K)/<i>T</i>]. Despite the suppressive effects of <i>I</i> on radical generation, the formation of FeSO<sub>4</sub> enhances the relevance of Fenton chemistry, highlighting its amplified role in sulfate-rich aerosol environments.</p>","PeriodicalId":15,"journal":{"name":"ACS Earth and Space Chemistry","volume":"9 3","pages":"662–670 662–670"},"PeriodicalIF":2.9000,"publicationDate":"2025-02-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://pubs.acs.org/doi/epdf/10.1021/acsearthspacechem.4c00362","citationCount":"0","resultStr":"{\"title\":\"Ionic Strength Effect in Fenton Reactions in the Presence of Sulfate and Its Influence on the Aqueous Particle Phase\",\"authors\":\"Daniele Scheres Firak, Thomas Schaefer, Celine Kula, Nazanin Taherkhani and Hartmut Herrmann*, \",\"doi\":\"10.1021/acsearthspacechem.4c0036210.1021/acsearthspacechem.4c00362\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p >Fenton chemistry [Fe(II) + H<sub>2</sub>O<sub>2</sub>] is a critical source of hydroxyl radicals (<sup>•</sup>OH) in deliquescent aerosols, yet its efficiency is significantly modulated by the high ionic strength (<i>I</i>) of these systems. This study investigates the influence of elevated sulfate concentrations on Fenton reactions under aerosol-relevant conditions. The isolated effect of ionic strength was first studied by using NaClO<sub>4</sub> as a model electrolyte. Results reveal that the Fenton reaction rate constant decreases sharply to 16 ± 1 M<sup>–1</sup> s<sup>–1</sup> until <i>I</i> = 2 M, increasing at higher <i>I</i> values. Fe(II) oxidation by dissolved O<sub>2</sub> increased to 282 ± 46 M<sup>–1</sup> s<sup>–1</sup> at <i>I</i> = 8 M, although dissolved O<sub>2</sub> concentrations are expected to decrease due to salting-out effects on oxygen. In Na<sub>2</sub>SO<sub>4</sub> solutions, Fe speciation shifts to FeSO<sub>4</sub>, resulting in enhanced rate constants, reaching 239 ± 21 M<sup>–1</sup> s<sup>–1</sup> at <i>I</i> = 2.7 M. Interestingly, Fe(II) oxidation by O<sub>2</sub> is negligible in Na<sub>2</sub>SO<sub>4</sub> solutions. The final OH yield remained unchanged in FeSO<sub>4</sub> solutions and decreased markedly in NaClO<sub>4</sub> solutions. Arrhenius expressions were derived for the Fenton reaction in 3.6 M NaClO<sub>4</sub> <i>k</i>(<i>T</i>) = (8.7 ± 0.8) × 10<sup>7</sup> × exp[(−4276 ± 520 K)/<i>T</i>] and the reaction in the presence of 1.2 M Na<sub>2</sub>SO<sub>4</sub>, <i>k</i>(<i>T</i>) = (7.5 ± 0.2) × 10<sup>9</sup> × exp[(−5153 ± 310 K)/<i>T</i>]. 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引用次数: 0
摘要
Fenton化学[Fe(II) + H2O2]是潮解气溶胶中羟基自由基(•OH)的重要来源,但其效率受到这些系统的高离子强度(I)的显著调节。在气溶胶相关条件下,研究了硫酸盐浓度升高对Fenton反应的影响。以氯化钠为模型电解质,首次研究了离子强度的孤立效应。结果表明,在I = 2 M之前,Fenton反应速率常数急剧下降至16±1 M - 1 s-1,在更高的I值时增加。在I = 8 M时,溶解的O2对Fe(II)的氧化增加到282±46 M - 1 s-1,尽管由于对氧的盐析作用,溶解的O2浓度预计会降低。在Na2SO4溶液中,Fe形态转变为FeSO4,导致速率常数提高,在I = 2.7 m时达到239±21 M-1 s-1。有趣的是,Fe(II)在Na2SO4溶液中被O2氧化可以忽略不计。最终OH产率在FeSO4溶液中保持不变,在NaClO4溶液中明显下降。得到Fenton反应在3.6 M NaClO4溶液中k(T) =(8.7±0.8)× 107 × exp[(- 4276±520 k)/T]和在1.2 M Na2SO4溶液中k(T) =(7.5±0.2)× 109 × exp[(- 5153±310 k)/T]的Arrhenius表达式。尽管I对自由基生成有抑制作用,但FeSO4的形成增强了Fenton化学的相关性,突出了其在富含硫酸盐的气溶胶环境中的放大作用。
Ionic Strength Effect in Fenton Reactions in the Presence of Sulfate and Its Influence on the Aqueous Particle Phase
Fenton chemistry [Fe(II) + H2O2] is a critical source of hydroxyl radicals (•OH) in deliquescent aerosols, yet its efficiency is significantly modulated by the high ionic strength (I) of these systems. This study investigates the influence of elevated sulfate concentrations on Fenton reactions under aerosol-relevant conditions. The isolated effect of ionic strength was first studied by using NaClO4 as a model electrolyte. Results reveal that the Fenton reaction rate constant decreases sharply to 16 ± 1 M–1 s–1 until I = 2 M, increasing at higher I values. Fe(II) oxidation by dissolved O2 increased to 282 ± 46 M–1 s–1 at I = 8 M, although dissolved O2 concentrations are expected to decrease due to salting-out effects on oxygen. In Na2SO4 solutions, Fe speciation shifts to FeSO4, resulting in enhanced rate constants, reaching 239 ± 21 M–1 s–1 at I = 2.7 M. Interestingly, Fe(II) oxidation by O2 is negligible in Na2SO4 solutions. The final OH yield remained unchanged in FeSO4 solutions and decreased markedly in NaClO4 solutions. Arrhenius expressions were derived for the Fenton reaction in 3.6 M NaClO4k(T) = (8.7 ± 0.8) × 107 × exp[(−4276 ± 520 K)/T] and the reaction in the presence of 1.2 M Na2SO4, k(T) = (7.5 ± 0.2) × 109 × exp[(−5153 ± 310 K)/T]. Despite the suppressive effects of I on radical generation, the formation of FeSO4 enhances the relevance of Fenton chemistry, highlighting its amplified role in sulfate-rich aerosol environments.
期刊介绍:
The scope of ACS Earth and Space Chemistry includes the application of analytical, experimental and theoretical chemistry to investigate research questions relevant to the Earth and Space. The journal encompasses the highly interdisciplinary nature of research in this area, while emphasizing chemistry and chemical research tools as the unifying theme. The journal publishes broadly in the domains of high- and low-temperature geochemistry, atmospheric chemistry, marine chemistry, planetary chemistry, astrochemistry, and analytical geochemistry. ACS Earth and Space Chemistry publishes Articles, Letters, Reviews, and Features to provide flexible formats to readily communicate all aspects of research in these fields.