Formation of Secondary Organic Aerosols by Germicidal Ultraviolet Light

被引:3
|
作者
Choi, Eureka [1 ]
Tan, Zhongchao [2 ]
Anderson, William A. [1 ]
机构
[1] Univ Waterloo, Dept Chem Engn, Waterloo, ON N2L 3G1, Canada
[2] Univ Waterloo, Dept Mech & Mechatron Engn, Waterloo, ON N2L 3G1, Canada
来源
ENVIRONMENTS | 2019年 / 6卷 / 02期
基金
加拿大自然科学与工程研究理事会;
关键词
fine particulate; PM2.5; UV disinfection; indoor air quality; toluene; INDOOR AIR; PHOTOOXIDATION;
D O I
10.3390/environments6020017
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 x 10(6) particles/m(3) for 5 min of UV exposure, to 163.2 x 10(6) particles/m(3) for 15 min of UV exposure, for toluene concentrations in the range of 55 to 85 mg/m(3). 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.
引用
收藏
页数:9
相关论文
共 50 条
  • [1] Formation and Transport of Secondary Contaminants Associated with Germicidal Ultraviolet Light Systems in an Occupied Classroom
    Park, Seongjun
    Won, Youngbo
    Rim, Donghyun
    ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2024, : 12051 - 12061
  • [2] Effect of ultraviolet germicidal irradiation on viral aerosols
    Walker, Christopher M.
    Ko, GwangPyo
    ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2007, 41 (15) : 5460 - 5465
  • [3] Chemical processes on the formation of secondary organic aerosols
    Wang, ZY
    Hao, LQ
    Zhang, WJ
    PROGRESS IN CHEMISTRY, 2005, 17 (04) : 732 - 739
  • [4] Studies on Formation of Aqueous Secondary Organic Aerosols
    Qi Qian
    Zhou Xuehua
    Wang Wenxing
    PROGRESS IN CHEMISTRY, 2014, 26 (2-3) : 458 - 466
  • [5] PARAMETERIZATION OF THE FORMATION POTENTIAL OF SECONDARY ORGANIC AEROSOLS
    GROSJEAN, D
    SEINFELD, JH
    ATMOSPHERIC ENVIRONMENT, 1989, 23 (08) : 1733 - 1747
  • [6] Inactivation of virus-containing aerosols by ultraviolet germicidal irradiation
    Tseng, CC
    Li, CS
    AEROSOL SCIENCE AND TECHNOLOGY, 2005, 39 (12) : 1136 - 1142
  • [7] HYPERSENSITIVITY OF FROZEN PHAGE TO GERMICIDAL ULTRAVIOLET LIGHT
    LEVINE, M
    FEDERATION PROCEEDINGS, 1965, 24 (2S15) : S85 - &
  • [8] Preventing biogenic secondary organic aerosols formation in India
    Azmi, Sahir
    Sharma, Mukesh
    ATMOSPHERIC ENVIRONMENT, 2022, 290
  • [9] Formation of secondary organic aerosols from the ozonolysis of dihydrofurans
    Diaz-de-Mera, Yolanda
    Aranda, Alfonso
    Bracco, Larisa
    Rodriguez, Diana
    Rodriguez, Ana
    ATMOSPHERIC CHEMISTRY AND PHYSICS, 2017, 17 (03) : 2347 - 2357
  • [10] Formation of secondary organic aerosols through photooxidation of isoprene
    Claeys, M
    Graham, B
    Vas, G
    Wang, W
    Vermeylen, R
    Pashynska, V
    Cafmeyer, J
    Guyon, P
    Andreae, MO
    Artaxo, P
    Maenhaut, W
    SCIENCE, 2004, 303 (5661) : 1173 - 1176