Measuring molecular singlet oxygen ( <sup>1</sup> O <sub>2</sub> *) from atmospheric photosensitizers: Intercomparison of techniques, irradiation setups, data analysis and protocol recommendations

Abstract. Molecular singlet oxygen (1O2*) is the first excited state of molecular oxygen (O2) and can be formed through indirect photochemistry during irradiation of chromophoric organic matter. Once formed in the particle and droplet phases in the atmosphere, 1O2* can be a competitive oxidant in the photochemical processing of organic matter. Now, as more researchers study the atmospheric photochemistry of 1O2*, establishing protocols by evaluating and comparing experimental setups across laboratories is becoming necessary. Here, we present 1O2* measurements from four photosensitizing molecules in four photoreactor setups at three research institutions, including two xenon lamps of different strengths and two multi-bulb UVA + UVB broadband systems. The production of 1O2* was investigated from perinaphthenone, lignin, and juglone, which are photosensitizers with atmospherically relevant light absorbing moieties, as well as from Rose Bengal, a standard photosensitizer. Two chemical actinometers, 2-nitrobenzaldehyde and p-nitroanisole/pyridine, were used to quantify photon fluxes and calculate rates of light absorbance for photosensitizers for each photoreactor. We compared two commonly used 1O2* quantification methods, chemical probe method using furfuryl alcohol, as well as direct 1O2* phosphorescence detection at 1270 nm. Rates of light absorbance across experimental setups for each photosensitizer ranged between 0.2 and 62 × 10−5 molphotons L−1 s−1, while 1O2* steady-state concentrations ranged between 0.01 and 129 × 10−11 M. Despite order of magnitude differences in rate of light absorbance and 1O2* steady state concentrations, normalizing to 1O2* quantum yields showed good inter-laboratory agreement but only for the sensitizers with high quantum yields: perinaphthenone (94 % ± 9 %–112 % ± 17 %) and for Rose Bengal (67 % ± 15 %–87 % ± 5 %). 1O2* quantum yields for lignin and juglone increased with decreasing irradiation wavelength, highlighting a wavelength-dependence. Finally, we make five recommendations to improve the accuracy and reproducibility of 1O2* measurements for the atmospheric chemistry community. These recommendations include considering wavelength-dependent quantum yields, avoiding suppression of 1O2*, controlling and reporting photoreactor temperature, considering light scattering from nanoparticles, and conducting control experiments. These recommendations can serve as guidelines to build future photoreactors as well as help standardize 1O2* measurements in studying photochemical processing of atmospheric aerosols and droplets.

Authors

Institutions

Publication Details

Journal
Atmospheric measurement techniques
Published
2026-06-17
DOI
https://doi.org/10.5194/amt-19-3961-2026
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Measuring molecular singlet oxygen ( 1 O 2 *) from atmospheric photosensitizers: Intercomparison of techniques, irradiation setups, data analysis and protocol recommendations

Zhongyu Guo, Belinda Heyne, Nory Mariño‐Ocampo, Cort Anastasio et al.
Atmospheric measurement techniques
Atmospheric chemistry and aerosols
article

Measuring molecular singlet oxygen ( 1 O 2 *) from atmospheric photosensitizers: Intercomparison of techniques, irradiation setups, data analysis and protocol recommendations

Zhongyu Guo, Belinda Heyne, Nory Mariño‐Ocampo, Cort Anastasio, Nadine Borduas‐Dedekind, Laura Marie Dahler Heinlein, Claudia Sardena, Keighan Gemmell, C. George, Emma A. Petersen-Sonn
article en

Abstract

Abstract. Molecular singlet oxygen (1O2*) is the first excited state of molecular oxygen (O2) and can be formed through indirect photochemistry during irradiation of chromophoric organic matter. Once formed in the particle and droplet phases in the atmosphere, 1O2* can be a competitive oxidant in the photochemical processing of organic matter. Now, as more researchers study the atmospheric photochemistry of 1O2*, establishing protocols by evaluating and comparing experimental setups across laboratories is becoming necessary. Here, we present 1O2* measurements from four photosensitizing molecules in four photoreactor setups at three research institutions, including two xenon lamps of different strengths and two multi-bulb UVA + UVB broadband systems. The production of 1O2* was investigated from perinaphthenone, lignin, and juglone, which are photosensitizers with atmospherically relevant light absorbing moieties, as well as from Rose Bengal, a standard photosensitizer. Two chemical actinometers, 2-nitrobenzaldehyde and p-nitroanisole/pyridine, were used to quantify photon fluxes and calculate rates of light absorbance for photosensitizers for each photoreactor. We compared two commonly used 1O2* quantification methods, chemical probe method using furfuryl alcohol, as well as direct 1O2* phosphorescence detection at 1270 nm. Rates of light absorbance across experimental setups for each photosensitizer ranged between 0.2 and 62 × 10−5 molphotons L−1 s−1, while 1O2* steady-state concentrations ranged between 0.01 and 129 × 10−11 M. Despite order of magnitude differences in rate of light absorbance and 1O2* steady state concentrations, normalizing to 1O2* quantum yields showed good inter-laboratory agreement but only for the sensitizers with high quantum yields: perinaphthenone (94 % ± 9 %–112 % ± 17 %) and for Rose Bengal (67 % ± 15 %–87 % ± 5 %). 1O2* quantum yields for lignin and juglone increased with decreasing irradiation wavelength, highlighting a wavelength-dependence. Finally, we make five recommendations to improve the accuracy and reproducibility of 1O2* measurements for the atmospheric chemistry community. These recommendations include considering wavelength-dependent quantum yields, avoiding suppression of 1O2*, controlling and reporting photoreactor temperature, considering light scattering from nanoparticles, and conducting control experiments. These recommendations can serve as guidelines to build future photoreactors as well as help standardize 1O2* measurements in studying photochemical processing of atmospheric aerosols and droplets.

Atmospheric measurement techniquesVol. 19(12)
Université Claude Bernard Lyon 1 (FR), Centre National de la Recherche Scientifique (FR), University of British Columbia (CA), University of Calgary (CA), Institut de Recherches sur la Catalyse et l'Environnement de Lyon (FR), University of California, Davis (US)
National Science Foundation, Agence Nationale de la Recherche, Université de Lyon, Natural Sciences and Engineering Research Council of Canada, University of British Columbia Graduate School
Openalex Percentile: Top 7%
Atmospheric chemistry and aerosols
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.