Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light

Ultraviolet (UV) light with a wavelength of 254 nm is known to be germicidal, and thus has been increasingly employed as a method of disinfection for indoor environments. Solar UV wavelengths (300 to 400 nm) are known to initiate the formation of secondary organic aerosol (SOA) particles from the ph...

Full description

Bibliographic Details
Main Authors: Eureka Choi, Zhongchao Tan, William A. Anderson
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Environments
Subjects:
Online Access:https://www.mdpi.com/2076-3298/6/2/17
_version_ 1798004013193494528
author Eureka Choi
Zhongchao Tan
William A. Anderson
author_facet Eureka Choi
Zhongchao Tan
William A. Anderson
author_sort Eureka Choi
collection DOAJ
description Ultraviolet (UV) light with a wavelength of 254 nm is known to be germicidal, and thus has been increasingly employed as a method of disinfection for indoor environments. Solar UV wavelengths (300 to 400 nm) are known to initiate the formation of secondary organic aerosol (SOA) particles from the photo-oxidation of volatile organic compounds (VOC) in the atmosphere, but germicidal wavelengths have not been extensively studied for indoor environments. In this work, toluene was exposed to 254 nm UV light in a laboratory photoreactor while varying the conditions of the air, the duration of UV exposure, and the duration of post-UV time. The number of particles formed in the fine particulate matter (PM2.5) size range was measured, and significant levels of particle formation were observed for UV exposure periods of as short as 5 min. The particle formation ranged from 2.4 &#215; 10<sup>6</sup> particles/m<sup>3</sup> for 5 min of UV exposure, to 163.2 &#215; 10<sup>6</sup> particles/m<sup>3</sup> for 15 min of UV exposure, for toluene concentrations in the range of 55 to 85 mg/m<sup>3</sup>. Particle formation was found to increase at a relative humidity of approximately 20% and higher. Variations in the initial number of particles present did not appear to have a significant effect on the particle formation, suggesting that nucleation was not a controlling factor under these conditions. However, tests in a commercial environment at much lower VOC concentrations and lower UV fluence rates showed no detectable PM2.5 formation, indicating that SOA formation during the intermittent use of germicidal UV may not significantly affect indoor air quality under normal conditions.
first_indexed 2024-04-11T12:16:49Z
format Article
id doaj.art-1c80954e052044e8a32b293c1a4cfcf9
institution Directory Open Access Journal
issn 2076-3298
language English
last_indexed 2024-04-11T12:16:49Z
publishDate 2019-01-01
publisher MDPI AG
record_format Article
series Environments
spelling doaj.art-1c80954e052044e8a32b293c1a4cfcf92022-12-22T04:24:16ZengMDPI AGEnvironments2076-32982019-01-01621710.3390/environments6020017environments6020017Formation of Secondary Organic Aerosols by Germicidal Ultraviolet LightEureka Choi0Zhongchao Tan1William A. Anderson2Department of Chemical Engineering, University of Waterloo, Waterloo, ON N2L 3G1, CanadaDepartment of Mechanical and Mechatronics Engineering, University of Waterloo, Waterloo, ON N2L 3G1, CanadaDepartment of Chemical Engineering, University of Waterloo, Waterloo, ON N2L 3G1, CanadaUltraviolet (UV) light with a wavelength of 254 nm is known to be germicidal, and thus has been increasingly employed as a method of disinfection for indoor environments. Solar UV wavelengths (300 to 400 nm) are known to initiate the formation of secondary organic aerosol (SOA) particles from the photo-oxidation of volatile organic compounds (VOC) in the atmosphere, but germicidal wavelengths have not been extensively studied for indoor environments. In this work, toluene was exposed to 254 nm UV light in a laboratory photoreactor while varying the conditions of the air, the duration of UV exposure, and the duration of post-UV time. The number of particles formed in the fine particulate matter (PM2.5) size range was measured, and significant levels of particle formation were observed for UV exposure periods of as short as 5 min. The particle formation ranged from 2.4 &#215; 10<sup>6</sup> particles/m<sup>3</sup> for 5 min of UV exposure, to 163.2 &#215; 10<sup>6</sup> particles/m<sup>3</sup> for 15 min of UV exposure, for toluene concentrations in the range of 55 to 85 mg/m<sup>3</sup>. Particle formation was found to increase at a relative humidity of approximately 20% and higher. Variations in the initial number of particles present did not appear to have a significant effect on the particle formation, suggesting that nucleation was not a controlling factor under these conditions. However, tests in a commercial environment at much lower VOC concentrations and lower UV fluence rates showed no detectable PM2.5 formation, indicating that SOA formation during the intermittent use of germicidal UV may not significantly affect indoor air quality under normal conditions.https://www.mdpi.com/2076-3298/6/2/17fine particulatePM2.5UV disinfectionindoor air qualitytoluene
spellingShingle Eureka Choi
Zhongchao Tan
William A. Anderson
Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light
Environments
fine particulate
PM2.5
UV disinfection
indoor air quality
toluene
title Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light
title_full Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light
title_fullStr Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light
title_full_unstemmed Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light
title_short Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light
title_sort formation of secondary organic aerosols by germicidal ultraviolet light
topic fine particulate
PM2.5
UV disinfection
indoor air quality
toluene
url https://www.mdpi.com/2076-3298/6/2/17
work_keys_str_mv AT eurekachoi formationofsecondaryorganicaerosolsbygermicidalultravioletlight
AT zhongchaotan formationofsecondaryorganicaerosolsbygermicidalultravioletlight
AT williamaanderson formationofsecondaryorganicaerosolsbygermicidalultravioletlight