Quantification and Mechanistic Investigation of the Spontaneous H2O2 Generation at the Interfaces of Salt-Containing Aqueous Droplets

There is now much evidence that OH radicals and H2O2 are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl–, Br–, I–), which are abundant in marine aerosols, on this H2O2 production. Droplets were generated via nebulizat...

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Published inJournal of the American Chemical Society Vol. 146; no. 12; pp. 8327 - 8334
Main Authors Angelaki, Maria, Carreira Mendes Da Silva, Yoan, Perrier, Sébastien, George, Christian
Format Journal Article
LanguageEnglish
Published American Chemical Society 27.03.2024
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Abstract There is now much evidence that OH radicals and H2O2 are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl–, Br–, I–), which are abundant in marine aerosols, on this H2O2 production. Droplets were generated via nebulization of water solutions containing Na2SO4, NaCl, NaBr, and NaI containing solutions, and H2O2 was monitored as a function of the salt concentration under atmospheric relevant conditions. The interfacial OH radical formation was also investigated by adding terephthalic acid (TA) to our salt solutions, and the product of its reaction with OH, hydroxy terephthalic acid (TAOH), was monitored. Finally, a mechanistic investigation was performed to examine the reactions participating in H2O2 production, and their respective contributions were quantified. Our results showed that only Br– contributes to the interfacial H2O2 formation, promoting the production by acting as an electron donor, while Na2SO4 and NaCl stabilized the droplets by only reducing their evaporation. TAOH was observed in the collected droplets and, for the first time, directly in the particle phase by means of online fluorescence spectroscopy, confirming the interfacial OH production. A mechanistic study suggests that H2O2 is formed by both OH and HO2 self-recombination, as well as HO2 reaction with H atoms. This work is expected to enhance our understanding of interfacial processes and assess their impact on climate, air quality, and health.
AbstractList There is now much evidence that OH radicals and H2O2 are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl–, Br–, I–), which are abundant in marine aerosols, on this H2O2 production. Droplets were generated via nebulization of water solutions containing Na2SO4, NaCl, NaBr, and NaI containing solutions, and H2O2 was monitored as a function of the salt concentration under atmospheric relevant conditions. The interfacial OH radical formation was also investigated by adding terephthalic acid (TA) to our salt solutions, and the product of its reaction with OH, hydroxy terephthalic acid (TAOH), was monitored. Finally, a mechanistic investigation was performed to examine the reactions participating in H2O2 production, and their respective contributions were quantified. Our results showed that only Br– contributes to the interfacial H2O2 formation, promoting the production by acting as an electron donor, while Na2SO4 and NaCl stabilized the droplets by only reducing their evaporation. TAOH was observed in the collected droplets and, for the first time, directly in the particle phase by means of online fluorescence spectroscopy, confirming the interfacial OH production. A mechanistic study suggests that H2O2 is formed by both OH and HO2 self-recombination, as well as HO2 reaction with H atoms. This work is expected to enhance our understanding of interfacial processes and assess their impact on climate, air quality, and health.
There is now much evidence that OH radicals and H 2 O 2 are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl – , Br – , I – ), which are abundant in marine aerosols, on this H 2 O 2 production. Droplets were generated via nebulization of water solutions containing Na 2 SO 4 , NaCl, NaBr, and NaI containing solutions, and H 2 O 2 was monitored as a function of the salt concentration under atmospheric relevant conditions. The interfacial OH radical formation was also investigated by adding terephthalic acid (TA) to our salt solutions, and the product of its reaction with OH, hydroxy terephthalic acid (TAOH), was monitored. Finally, a mechanistic investigation was performed to examine the reactions participating in H 2 O 2 production, and their respective contributions were quantified. Our results showed that only Br – contributes to the interfacial H 2 O 2 formation, promoting the production by acting as an electron donor, while Na 2 SO 4 and NaCl stabilized the droplets by only reducing their evaporation. TAOH was observed in the collected droplets and, for the first time, directly in the particle phase by means of online fluorescence spectroscopy, confirming the interfacial OH production. A mechanistic study suggests that H 2 O 2 is formed by both OH and HO 2 self-recombination, as well as HO 2 reaction with H atoms. This work is expected to enhance our understanding of interfacial processes and assess their impact on climate, air quality, and health.
There is now much evidence that OH radicals and H2O2 are spontaneously generated at the air-water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl-, Br-, I-), which are abundant in marine aerosols, on this H2O2 production. Droplets were generated via nebulization of water solutions containing Na2SO4, NaCl, NaBr, and NaI containing solutions, and H2O2 was monitored as a function of the salt concentration under atmospheric relevant conditions. The interfacial OH radical formation was also investigated by adding terephthalic acid (TA) to our salt solutions, and the product of its reaction with OH, hydroxy terephthalic acid (TAOH), was monitored. Finally, a mechanistic investigation was performed to examine the reactions participating in H2O2 production, and their respective contributions were quantified. Our results showed that only Br- contributes to the interfacial H2O2 formation, promoting the production by acting as an electron donor, while Na2SO4 and NaCl stabilized the droplets by only reducing their evaporation. TAOH was observed in the collected droplets and, for the first time, directly in the particle phase by means of online fluorescence spectroscopy, confirming the interfacial OH production. A mechanistic study suggests that H2O2 is formed by both OH and HO2 self-recombination, as well as HO2 reaction with H atoms. This work is expected to enhance our understanding of interfacial processes and assess their impact on climate, air quality, and health.There is now much evidence that OH radicals and H2O2 are spontaneously generated at the air-water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl-, Br-, I-), which are abundant in marine aerosols, on this H2O2 production. Droplets were generated via nebulization of water solutions containing Na2SO4, NaCl, NaBr, and NaI containing solutions, and H2O2 was monitored as a function of the salt concentration under atmospheric relevant conditions. The interfacial OH radical formation was also investigated by adding terephthalic acid (TA) to our salt solutions, and the product of its reaction with OH, hydroxy terephthalic acid (TAOH), was monitored. Finally, a mechanistic investigation was performed to examine the reactions participating in H2O2 production, and their respective contributions were quantified. Our results showed that only Br- contributes to the interfacial H2O2 formation, promoting the production by acting as an electron donor, while Na2SO4 and NaCl stabilized the droplets by only reducing their evaporation. TAOH was observed in the collected droplets and, for the first time, directly in the particle phase by means of online fluorescence spectroscopy, confirming the interfacial OH production. A mechanistic study suggests that H2O2 is formed by both OH and HO2 self-recombination, as well as HO2 reaction with H atoms. This work is expected to enhance our understanding of interfacial processes and assess their impact on climate, air quality, and health.
There is now much evidence that OH radicals and H$_2$O$_2$ are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl$^–$, Br$^–$, I$^–$), which are abundant in marine aerosols, on this H$_2$O$_2$ production. Droplets were generated via nebulization of water solutions containing Na$_2$SO$_4$, NaCl, NaBr, and NaI containing solutions, and H2O2 was monitored as a function of the salt concentration under atmospheric relevant conditions. The interfacial OH radical formation was also investigated by adding terephthalic acid (TA) to our salt solutions, and the product of its reaction with OH, hydroxy terephthalic acid (TAOH), was monitored. Finally, a mechanistic investigation was performed to examine the reactions participating in H$_2$O$_2$ production, and their respective contributions were quantified. Our results showed that only Br– contributes to the interfacial H$_2$O$_2$ formation, promoting the production by acting as an electron donor, while Na$_2$SO$_4$ and NaCl stabilized the droplets by only reducing their evaporation. TAOH was observed in the collected droplets and, for the first time, directly in the particle phase by means of online fluorescence spectroscopy, confirming the interfacial OH production. A mechanistic study suggests that H$_2$O$_2$ is formed by both OH and HO$_2$ self-recombination, as well as HO$_2$ reaction with H atoms. This work is expected to enhance our understanding of interfacial processes and assess their impact on climate, air quality, and health
There is now much evidence that OH radicals and H₂O₂ are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the effect of halide anions (Cl–, Br–, I–), which are abundant in marine aerosols, on this H₂O₂ production. Droplets were generated via nebulization of water solutions containing Na₂SO₄, NaCl, NaBr, and NaI containing solutions, and H₂O₂ was monitored as a function of the salt concentration under atmospheric relevant conditions. The interfacial OH radical formation was also investigated by adding terephthalic acid (TA) to our salt solutions, and the product of its reaction with OH, hydroxy terephthalic acid (TAOH), was monitored. Finally, a mechanistic investigation was performed to examine the reactions participating in H₂O₂ production, and their respective contributions were quantified. Our results showed that only Br– contributes to the interfacial H₂O₂ formation, promoting the production by acting as an electron donor, while Na₂SO₄ and NaCl stabilized the droplets by only reducing their evaporation. TAOH was observed in the collected droplets and, for the first time, directly in the particle phase by means of online fluorescence spectroscopy, confirming the interfacial OH production. A mechanistic study suggests that H₂O₂ is formed by both OH and HO₂ self-recombination, as well as HO₂ reaction with H atoms. This work is expected to enhance our understanding of interfacial processes and assess their impact on climate, air quality, and health.
Author Perrier, Sébastien
Angelaki, Maria
George, Christian
Carreira Mendes Da Silva, Yoan
AuthorAffiliation Université Claude Bernard Lyon 1, CNRS, IRCELYON, UMR 5256
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  surname: George
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  email: christian.george@ircelyon.univ-lyon1.fr
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Snippet There is now much evidence that OH radicals and H2O2 are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the...
There is now much evidence that OH radicals and H2O2 are spontaneously generated at the air-water interface of atmospheric aerosols. Here, we investigated the...
There is now much evidence that OH radicals and H₂O₂ are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated the...
There is now much evidence that OH radicals and H$_2$O$_2$ are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we...
There is now much evidence that OH radicals and H 2 O 2 are spontaneously generated at the air–water interface of atmospheric aerosols. Here, we investigated...
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SubjectTerms air quality
Atmospheric and Oceanic Physics
atomization
Chemical Sciences
climate
evaporation
fluorescence emission spectroscopy
liquid-air interface
or physical chemistry
Physics
salt concentration
sodium bromide
Theoretical and
Title Quantification and Mechanistic Investigation of the Spontaneous H2O2 Generation at the Interfaces of Salt-Containing Aqueous Droplets
URI http://dx.doi.org/10.1021/jacs.3c14040
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Volume 146
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