Secondary organic aerosol (SOA) is formed from the atmospheric oxidation of gas-phase organic compounds leading to the formation of particle mass. Gasoline-and diesel-powered …
Civil aviation is fast-growing (about+ 5% every year), mainly driven by the developing economies and globalisation. Its impact on the environment is heavily debated, particularly …
NO x lifetime relates nonlinearly to its own concentration; therefore, by observing how NO x lifetime changes with changes in its concentration, inferences can be made about the …
The present paper reviews existing knowledge with regard to Organic Aerosol (OA) of importance for global climate modelling and defines critical gaps needed to reduce the …
This comprehensive text describes the atmospheric processes, numerical methods, and computational techniques required for a scientist to successfully study air pollution and …
We discuss the use of a two-dimensional volatility-oxidation space (2-D-VBS) to describe organic-aerosol chemical evolution. The space is built around two coordinates, volatility and …
AJ Macpherson, T Uhr - Science, 2004 - science.org
The enormous number of commensal bacteria in the lower intestine of vertebrates share abundant molecular patterns used for innate immune recognition of pathogenic bacteria. We …
An equation that can successfully parameterize gas-particle partitioning is K p (m 3 μg− 1)=(F/TSP)/A, where K p is a partitioning constant, TSP (μg m− 3) is the concentration of total …
Most primary organic-particulate emissions are semivolatile; thus, they partially evaporate with atmospheric dilution, creating substantial amounts of low-volatility gas-phase material …