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Photochemical emissions of HONO, NO2 and NO from the soil surface under simulated sunlight
Abstract Emissions of HONO, NO2 and NO from different soils under simulated sunlight were investigated using a flow reactor at ambient pressure. Enhanced emissions of HONO, NO2 and NO were observed when soils were exposed to the simulated sunlight. NO3 − and NO2 − partly contributed to the HONO and NO formations, whereas NH4 + and NH2OH played minor roles in HONO, NO2 and NO emissions from the soil. The emission flux densities of HONO (F HONO), NO2 () and NO (F NO) significantly depended on environmental conditions, including irradiation intensity, relative humidity (RH), temperature and pH. F HONO, and F NO linearly increased with increasing irradiation intensity in the range of 0–320 W/m2. Maximum values of F HONO, and F NO appeared at RH = 55%. F HONO and F NO increased while decreased with increasing the temperature in the range of 278–338 K. Maximum F HONO and values appeared at pH = 8 while larger F NO values occurred at pH of 2 and 8. Atmospheric implications about the photochemical emission of HONO from soil contributing to HONO in the atmosphere were also discussed.
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Highlights Light significantly enhanced HONO, NO2 and NO emissions from soils. NO3 − and NO2 − partly contributed to the HONO and NO emissions from the soil. HONO, NO2 and NO emission flux densities depended on the environmental conditions.
Photochemical emissions of HONO, NO2 and NO from the soil surface under simulated sunlight
Abstract Emissions of HONO, NO2 and NO from different soils under simulated sunlight were investigated using a flow reactor at ambient pressure. Enhanced emissions of HONO, NO2 and NO were observed when soils were exposed to the simulated sunlight. NO3 − and NO2 − partly contributed to the HONO and NO formations, whereas NH4 + and NH2OH played minor roles in HONO, NO2 and NO emissions from the soil. The emission flux densities of HONO (F HONO), NO2 () and NO (F NO) significantly depended on environmental conditions, including irradiation intensity, relative humidity (RH), temperature and pH. F HONO, and F NO linearly increased with increasing irradiation intensity in the range of 0–320 W/m2. Maximum values of F HONO, and F NO appeared at RH = 55%. F HONO and F NO increased while decreased with increasing the temperature in the range of 278–338 K. Maximum F HONO and values appeared at pH = 8 while larger F NO values occurred at pH of 2 and 8. Atmospheric implications about the photochemical emission of HONO from soil contributing to HONO in the atmosphere were also discussed.
Graphical abstract Display Omitted
Highlights Light significantly enhanced HONO, NO2 and NO emissions from soils. NO3 − and NO2 − partly contributed to the HONO and NO emissions from the soil. HONO, NO2 and NO emission flux densities depended on the environmental conditions.
Photochemical emissions of HONO, NO2 and NO from the soil surface under simulated sunlight
Yang, Wangjin (author) / Yuan, Hua (author) / Han, Chong (author) / Yang, He (author) / Xue, Xiangxin (author)
Atmospheric Environment ; 234
2020-05-07
Article (Journal)
Electronic Resource
English
HONO , NO<inf>2</inf> , NO , Photochemical emission , Soil
Wood surface discolouration due to simulated indoor sunlight exposure
British Library Online Contents | 2008
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