Results of this measurement campaign indicate that alcohol fuels (E85, E100) significantly reduce both primary particulate emissions as well as subsequent
secondary aerosol formation in the atmosphere when compared emissions of gasoline fuels.
Timonen, H., Karjalainen, P., Saukko, E., Saarikoski, S., Aakko - Saksa, P., Simonen, P., Murtonen, T., Dal Maso, M., Kuuluvainen, H., Bloss, M., Ahlberg, E., Svenningsson, B., Pagels, J., Brune, W. H., Keskinen, J., Worsnop, D. R., Hillamo, R., and Rönkkö, T.: Influence of fuel ethanol content on primary emissions and
secondary aerosol formation potential for a modern flex - fuel gasoline vehicle, Atmos.
Secondary aerosol formation from atmospheric reactions of aliphatic amines.
Not exact matches
They also play a role in the
formation of
secondary organic
aerosols — air pollutants produced when sunlight, organic molecules and airborne chemicals come together and interact.
Yet, the factors that influence the
formation of these
aerosols, known as
secondary organic
aerosol or SOA, are often assumed.
A study published April 7 in PNAS Online Early Edition describes how a team of scientists, including researchers from the University of California, Davis, showed that vapor losses to the walls of laboratory chambers can suppress the
formation of
secondary organic
aerosol, which in turn has contributed to the underprediction of SOA in climate and air quality models.
In one of the first studies of its kind, scientists have found that tar sands production in Canada is one of North America's largest sources of
secondary organic
aerosols — air pollutants that affect the climate, cloud
formation and public health.
Laboratory chamber walls have been stealing vapors, causing researchers to underestimate the
formation of
secondary organic
aerosol in the atmosphere.
Even though open windows bring in more ozone from outside, the reduction in the indoor limonene concentration and SOA
formation strength more than make up for it, as less
secondary organic
aerosol is formed inside.
In research recently published in Environmental Science & Technology, Waring describes the role of limonene, the organic compound that gives cleaners and air fresheners an orange scent and acts as a solvent, in the
formation of
secondary organic
aerosols.
By adjusting elements of the test, such as the air exchange rate, which is the number of times per hour indoor air is replaced by outdoor air, as well as the concentrations of terpene and ozone in the chamber, the group was able to ascertain how those variables each affected the
formation of
secondary organic
aerosols.
With 18 different scenarios tested, the team calculated a range of peak
formation of
secondary organic
aerosols when typical concentrations of limonene were introduced to ozone - rich environments with a range of air exchange rates.
«Nighttime chemical evolution of
aerosol and trace gases in a power plant plume: Implications for
secondary organic nitrate and organosulfate
aerosol formation, NO3 radical chemistry, and N2O5 heterogeneous hydrolysis.»
A large portion of
secondary organic
aerosols - tiny particles in the air we breathe that contribute to cloud
formation and precipitation - arise from a combination of man - made pollution and molecules given off by plant matter.
Session Description: Recent laboratory and field studies provide new insights into the
formation, growth, phase, viscosity, and volatility of
secondary organic
aerosols (SOA).
Formation of nitrogen - and sulfur - containing light - absorbing compounds accelerated by evaporation of water from
secondary organic
aerosols
The
formation, properties and impact of
secondary organic
aerosol: Current and emerging issues
However, because of its acidity, H2SO4 (and potentially MSA) can enhance the
formation and growth of
secondary organic
aerosol (SOA) from organic compounds (5, 44, 45), including those produced by homogeneous nucleation of low - volatility species (46).
Effect of pellet boiler exhaust on
secondary organic
aerosol formation from α - pinene.
The successful candidate will study
secondary organic
aerosol (SOA)
formation from the oxidation of biogenic volatile organic compounds (VOCs).
Emissions of carbon dioxide, methane, nitrous oxide and of reactive gases such as sulphur dioxide, nitrogen oxides, carbon monoxide and hydrocarbons, which lead to the
formation of
secondary pollutants including
aerosol particles and tropospheric ozone, have increased substantially in response to human activities.
The present 3 - D modeling study focuses on
aerosol chemical composition change since preindustrial times considering the
secondary organic
aerosol formation together with all other main
aerosol components including nitrate.
My studies range from detailed
aerosol processes such as the
formation of
secondary organic
aerosols (SOA), to centennial time scale climate variability related to natural variability and external forcings.