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Updated: Sep 12, 2025

Production and Measurement of Organic Particulate Matter in the Harvard Environmental Chamber
Published on: November 18, 2018
Natural sources exert substantially greater influence on atmospheric ozone formation during high-ozone episodes in a
Tao Yang1, Baoshuang Liu2, Sen Li3
1China Automotive Technology & Research Center Co. Ltd., Beijing, 100176, China; Key Laboratory of Urban Air Particulate Pollution Prevention and Control of Ministry of Ecology and Environment, College of Environmental Science and Engineering, Nankai University, Tianjin, 300350, China.
Abstract:
Atmospheric ozone (O3) formation mechanisms remain challenging to clarify through conventional approaches that rely on the observed or initial volatile organic compound (VOC) concentration data, as they fail to capture the dynamic photochemical consumption processes. This study presents a novel consumption-based methodology that quantifies photochemically consumed VOCs and their critical sources during the O3 formation, providing unprecedented insights into the pollution mechanisms. Through systematic analysis of 17 typical high O3 episodes in 2020 in Zhumadian, China, the results showed that the photochemical losses of alkenes had the most substantial impact on the O3 formation, with a contribution of ∼94.9 % to the total O3 formation potential (OFP) of the consumed VOCs. The losses and OFP values of isoprene and ethylene, which are primarily derived from biogenic and combustion emissions, respectively, were markedly higher than those of any other VOC species. Biogenic emissions (∼55.8 %) and combustion emissions (∼16.8 %) were the primary contributing sources to the consumed VOCs during these O3 episodes. The OFP of the consumed VOCs derived from biogenic emissions (47.3 %) and combustion emissions (27.6 %) contributed the highest to the total OFP of the consumed VOCs derived from all the emission sources. Therefore, natural sources could exert clearly greater impacts on atmospheric O3 formation during the high O3 episodes. These findings provide a transformative understanding of O3 formation kinetics and establish a new paradigm for urban air quality management that must account for biogenic-anthropogenic interactions.
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