Ultrafine aerosol formation via ion‐mediated nucleation
By Fangqun Yu, R. Turco. 2000
381 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/87b50c97c87d422eff0931c34455b0ac67d00f3d
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In Atmospheric Science
- Markku Kulmala
- Richard Harrison
- V. Kerminen
- K. Carslaw
- Tuukka Petäjä
- K. Lehtinen
- Fangqun Yu
- J. Kirkby
In Global and Planetary Change
Citations in the corpus
- Atmospheric new particle formation and growth: review of field observations (2018, background): “First, the condensation growth of charged aerosol particles is expected to be enhanced compared with similar-size neutral particles (Yu and Turco 2000, Nadykto and Yu 2003, Lushnikov and Kulmala 2004).”
- Annual and size dependent variation of growth rates and ion concentrations in boreal forest (2005, background): “The idea of this analysis was to study the possible effect of charge on growth rates as pro- posed by Yu and Turco (2000) and Laakso et al. (2003a).”
- Cosmic Rays and Climate (2005, background): “The presence of charge stabilises the embryonic cluster through Coulomb attraction, and reduces the critical size—a process known as ion induced nucleation [105, 106, 107].”
- The Sun and the Earth’s Climate (2007, background): “Some observational evidence (Yu and Turco, 2000) suggests that charged molecular clusters grow faster than neutral clusters and chemical box models (Yu and Turco, 2001) have”
- Ion‐mediated nucleation in the atmosphere: Key controlling parameters, implications, and look‐up table (2010, methodology): “[8] Built upon an earlier version of the IMN model [ Yu and Turco, 1997, 2000, 2001 ], Yu [2006] developed a second-generation IMN model which incorporates new thermodynamic data [Froyd, 2002; Wilhelm et al., 2004] and physical algorithms [Nadykto and Yu, 2003; Yu, 2005] and explicitly treats the ev”
- Ambient nano and ultrafine particles from motor vehicle emissions: Characteristics, ambient processing and implications on human exposure (2008, background): “Yu and Turco (2000; 2001) showed that charged molecular clusters can grow significantly faster than neutral clusters and achieve stable observable sizes.”
- Altitude variations of cosmic ray induced production of aerosols: Implications for global cloudiness and climate (2002, background): “The organics species may play an important role in growing the CN into the size of CCN. YU: ALTITUDE VARIATIONS SIA typical tropospheric conditions [Yu and Turco, 2000, 2001].”
- Solar activity and terrestrial climate: an analysis of some purported correlations (2003, neutral): “According to current theory (e.g. Yu and Turco 2000) the build-up of cloud condensation nuclei is comp leted within less than a day after an increase of GCRI.”
- Multicomponent aerosol dynamics model UHMA: model development and validation (2004, background): “In addition, compared to corresponding neutral clusters, charged clusters formed on ions are more stable and can grow faster, thus supporting the ion mediated nucleation mechanism (Yu and Turco, 2000).”
- Exposure Assessment for Atmospheric Ultrafine Particles (UFPs) and Implications in Epidemiologic Research (2005, background): “A variety of different nucleation mechanisms have been proposed for the atmosphere, including binary water–sulfuric acid nucleation (Kulmala and Laaksonen 1990), ternary water–sulfuric acid–ammonia nucleation (Kulmala et al. 2000), and ioninduced nucleation (Yu and Turco 2000).”
- Initial steps of aerosol growth (2004, positive): “The presence of ions – and electric charge on particles will enhance the growth rates of very small (nanometer size) aerosol particles and air ions (Yu and Turco, 2000; Laakso et al., 2003; Nadykto and Yu, 2003; Lushnikov and Kulmala , 2004).”
- Ion‐aerosol‐cloud processes in the lower atmosphere (2003, background): “In subsequent studies of the background atmosphere [Yu and Turco, 2000] it was found that charged molecular clusters can grow significantly faster than neutral clusters.”
- New parameterization of sulfuric acid‐ammonia‐water ternary nucleation rates at tropospheric conditions (2007, background): “Therefore other nucleation mechanisms, such as ion-induced nucleation [ Yu and Turco, 2000; Lee et al., 2003; Laakso et al., 2004; Lovejoy et al., 2004; Eisele et al., 2006; Iida et al., 2006; Yu, 2006a], participation of sulfuric acid in kinetic nucleation and activation mechanism [Kulmala et al.,”