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      Phase Behavior of Internal Mixtures of Hydrocarbon-like Primary Organic Aerosol and Secondary Aerosol Based on Their Differences in Oxygen-to-Carbon Ratios

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          Abstract

          The phase behavior, the number and type of phases, in atmospheric particles containing mixtures of hydrocarbon-like organic aerosol (HOA) and secondary organic aerosol (SOA) is important for predicting their impacts on air pollution, human health, and climate. Using a solvatochromic dye and fluorescence microscopy, we determined the phase behavior of 11 HOA proxies (O/C = 0–0.29) each mixed with 7 different SOA materials generated in environmental chambers (O/C 0.4–1.08), where O/C represents the average oxygen-to-carbon atomic ratio. Out of the 77 different HOA + SOA mixtures studied, we observed two phases in 88% of the cases. The phase behavior was independent of relative humidity over the range between 90% and <5%. A clear trend was observed between the number of phases and the difference between the average O/C ratios of the HOA and SOA components (ΔO/C). Using a threshold ΔO/C of 0.265, we were able to predict the phase behavior of 92% of the HOA + SOA mixtures studied here, with one-phase particles predicted for ΔO/C < 0.265 and two-phase particles predicted for ΔO/C ≥ 0.265. The threshold ΔO/C value provides a relatively simple and computationally inexpensive framework for predicting the number of phases in internal SOA and HOA mixtures in atmospheric models.

          Abstract

          Studying the internal mixtures of primary organic aerosol (POA) and secondary organic aerosol (SOA) materials, we show that most POA + SOA mixtures exhibit phase-separated particles and that this miscibility gap can be predicted using the difference in the average elemental oxygen-to-carbon ratio of the organic components.

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          The contribution of outdoor air pollution sources to premature mortality on a global scale.

          Assessment of the global burden of disease is based on epidemiological cohort studies that connect premature mortality to a wide range of causes, including the long-term health impacts of ozone and fine particulate matter with a diameter smaller than 2.5 micrometres (PM2.5). It has proved difficult to quantify premature mortality related to air pollution, notably in regions where air quality is not monitored, and also because the toxicity of particles from various sources may vary. Here we use a global atmospheric chemistry model to investigate the link between premature mortality and seven emission source categories in urban and rural environments. In accord with the global burden of disease for 2010 (ref. 5), we calculate that outdoor air pollution, mostly by PM2.5, leads to 3.3 (95 per cent confidence interval 1.61-4.81) million premature deaths per year worldwide, predominantly in Asia. We primarily assume that all particles are equally toxic, but also include a sensitivity study that accounts for differential toxicity. We find that emissions from residential energy use such as heating and cooking, prevalent in India and China, have the largest impact on premature mortality globally, being even more dominant if carbonaceous particles are assumed to be most toxic. Whereas in much of the USA and in a few other countries emissions from traffic and power generation are important, in eastern USA, Europe, Russia and East Asia agricultural emissions make the largest relative contribution to PM2.5, with the estimate of overall health impact depending on assumptions regarding particle toxicity. Model projections based on a business-as-usual emission scenario indicate that the contribution of outdoor air pollution to premature mortality could double by 2050.
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            Evolution of organic aerosols in the atmosphere.

            Organic aerosol (OA) particles affect climate forcing and human health, but their sources and evolution remain poorly characterized. We present a unifying model framework describing the atmospheric evolution of OA that is constrained by high-time-resolution measurements of its composition, volatility, and oxidation state. OA and OA precursor gases evolve by becoming increasingly oxidized, less volatile, and more hygroscopic, leading to the formation of oxygenated organic aerosol (OOA), with concentrations comparable to those of sulfate aerosol throughout the Northern Hemisphere. Our model framework captures the dynamic aging behavior observed in both the atmosphere and laboratory: It can serve as a basis for improving parameterizations in regional and global models.
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              Organic aerosol and global climate modelling: a review

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                Author and article information

                Journal
                Environ Sci Technol
                Environ Sci Technol
                es
                esthag
                Environmental Science & Technology
                American Chemical Society
                0013-936X
                1520-5851
                16 March 2022
                05 April 2022
                : 56
                : 7
                : 3960-3973
                Affiliations
                []Department of Chemistry, University of British Columbia , 2036 Main Mall, Vancouver, British Columbia V6T1Z1, Canada
                []Laboratory of Environmental Chemistry, Paul Scherrer Institute , 5232 Villigen, Switzerland
                [§ ]Institute for Environmental and Climate Research, Jinan University , Guangzhou 511443, China
                []John A. Paulson School of Engineering and Applied Sciences, Harvard University , Cambridge, Massachusetts 02138, United States
                []Center for the Environment, Harvard University , Cambridge, Massachusetts 02138, United States
                [# ]Department of Earth and Planetary Sciences, Harvard University , Cambridge, Massachusetts 02138, United States
                Author notes
                Author information
                https://orcid.org/0000-0002-7059-6765
                https://orcid.org/0000-0003-4192-1888
                https://orcid.org/0000-0002-8996-7554
                https://orcid.org/0000-0001-5922-9000
                https://orcid.org/0000-0002-5621-2323
                Article
                10.1021/acs.est.1c07691
                8988305
                35294833
                041719da-5266-475a-8a45-8f3053eb11cb
                © 2022 The Authors. Published by American Chemical Society

                Permits non-commercial access and re-use, provided that author attribution and integrity are maintained; but does not permit creation of adaptations or other derivative works ( https://creativecommons.org/licenses/by-nc-nd/4.0/).

                History
                : 11 November 2021
                : 03 March 2022
                : 02 March 2022
                Funding
                Funded by: National Science Foundation, doi 10.13039/100000001;
                Award ID: ECS-2003368
                Funded by: UBC Work Lean International Undergraduate Research Awards, doi NA;
                Award ID: 111108
                Funded by: Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada, doi 10.13039/501100002790;
                Award ID: RGPIN/04441-2016
                Funded by: H2020 Marie Sklodowska-Curie Actions, doi 10.13039/100010665;
                Award ID: 890200
                Funded by: Center for the Environment, Harvard University, doi 10.13039/100008263;
                Award ID: NA
                Categories
                Article
                Custom metadata
                es1c07691
                es1c07691

                General environmental science
                air pollution,phase separation,organic aerosol particles,human health,oxygen-to-carbon ratio,secondary organic aerosol

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