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      Characteristics of marine shipping emissions at berth: profiles for particulate matter and volatile organic compounds

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          Abstract

          <p><strong>Abstract.</strong> Emissions from ships at berth play an important role regarding the exposure of high density human populations to atmospheric pollutants in port areas; however, these emissions are not well understood. In this study, volatile organic compounds (VOCs) and particle emissions from 20 container ships at berth were sampled and analyzed during the “fuel switch” period at Jingtang Port in Hebei Province, China. VOCs and particles were analyzed using a gas chromatography-mass spectrometer (GC-MS) and a single particle aerosol mass spectrometer (SPAMS), respectively. VOC analysis showed that alkanes and aromatics, especially benzene, toluene and heavier compounds e.g., <span class="inline-formula"><i>n</i></span>-heptane, <span class="inline-formula"><i>n</i></span>-octane and <span class="inline-formula"><i>n</i></span>-nonane, dominated the total identified species. Secondary organic aerosol (SOA) yields and ozone (<span class="inline-formula">O<sub>3</sub></span>) forming potential were 0.017<span class="thinspace"></span><span class="inline-formula">±</span><span class="thinspace"></span>0.007<span class="thinspace"></span>g<span class="thinspace"></span>SOA<span class="thinspace"></span>g<span class="inline-formula"><sup>−1</sup></span><span class="thinspace"></span>VOCs and 2.63<span class="thinspace"></span><span class="inline-formula">±</span><span class="thinspace"></span>0.37<span class="thinspace"></span>g<span class="thinspace"></span><span class="inline-formula">O<sub>3</sub></span><span class="thinspace"></span>g<span class="inline-formula"><sup>−1</sup></span><span class="thinspace"></span>VOCs, respectively. Both positive and negative ion mass spectra from individual ships were derived and the intensity of specific ions were quantified. Results showed that elemental carbon (35.74<span class="thinspace"></span>%), elemental carbon–organic carbon mixtures (33.95<span class="thinspace"></span>%) and Na-rich particles (21.12<span class="thinspace"></span>%) were major classes, comprising 90.7<span class="thinspace"></span>% of the particles observed. Particles from ship auxiliary engines were in the 0.2 to 2.5<span class="thinspace"></span><span class="inline-formula">µ</span>m size range, with a peak occurring at around 0.4<span class="thinspace"></span><span class="inline-formula">µ</span>m. The issue of using vanadium (V) as tracer element was examined, and it was found that V was not a proper tracer of ship emissions when using low sulfur content diesel oil. The average percentage of sulfate particles observed in shipping emissions before and after switching to marine diesel oil remained unchanged at 24<span class="thinspace"></span>%. Under certain wind conditions, when berths were upwind of emission sources, the ratios before and after 1 January were 35 and 27<span class="thinspace"></span>% respectively. The impact of atmospheric stability was discussed based on PM<span class="inline-formula"><sub>2.5</sub></span> and primary pollutant (carbon monoxide) concentration. With a background of frequent haze episodes and complex mechanisms of particulate accumulation and secondary formation, the impact of atmospheric stability is believed to have been weak on the sulfate contribution from shipping emissions. The results from this study provide robust support for port area air quality assessment and source apportionment.</p>

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          Persistent sulfate formation from London Fog to Chinese haze.

          Sulfate aerosols exert profound impacts on human and ecosystem health, weather, and climate, but their formation mechanism remains uncertain. Atmospheric models consistently underpredict sulfate levels under diverse environmental conditions. From atmospheric measurements in two Chinese megacities and complementary laboratory experiments, we show that the aqueous oxidation of SO2 by NO2 is key to efficient sulfate formation but is only feasible under two atmospheric conditions: on fine aerosols with high relative humidity and NH3 neutralization or under cloud conditions. Under polluted environments, this SO2 oxidation process leads to large sulfate production rates and promotes formation of nitrate and organic matter on aqueous particles, exacerbating severe haze development. Effective haze mitigation is achievable by intervening in the sulfate formation process with enforced NH3 and NO2 control measures. In addition to explaining the polluted episodes currently occurring in China and during the 1952 London Fog, this sulfate production mechanism is widespread, and our results suggest a way to tackle this growing problem in China and much of the developing world.
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            Production flux of sea spray aerosol

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              Marine aerosol, sea-salt, and the marine sulphur cycle: a short review

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                Author and article information

                Journal
                Atmospheric Chemistry and Physics
                Atmos. Chem. Phys.
                Copernicus GmbH
                1680-7324
                2018
                July 06 2018
                : 18
                : 13
                : 9527-9545
                Article
                10.5194/acp-18-9527-2018
                c31298db-b586-41d0-be25-3ce4f0e53b32
                © 2018

                https://creativecommons.org/licenses/by/4.0/

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