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2014
DOI: 10.1016/j.atmosenv.2014.04.002
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Influence of trans-boundary biomass burning impacted air masses on submicron particle number concentrations and size distributions

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Cited by 17 publications
(10 citation statements)
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References 59 publications
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“…For instance, in the photochemical aging experiment for wheat straw burning (Fig. 3c), the growth rate of particles was 18 nm h −1 in the first 0.5 h and decreased to ∼ 1 nm h −1 during the following 4.5 h. The size distribution of aged aerosol particles in our study is similar to those of ambient particles under the severe biomass burning impact during haze events (Betha et al, 2014;Niu et al, 2016). Figure 4 shows the chemical evolution of aerosol particles during the 5 h photochemical aging of wheat straw burning.…”
Section: Evolution Of Particlessupporting
confidence: 65%
“…For instance, in the photochemical aging experiment for wheat straw burning (Fig. 3c), the growth rate of particles was 18 nm h −1 in the first 0.5 h and decreased to ∼ 1 nm h −1 during the following 4.5 h. The size distribution of aged aerosol particles in our study is similar to those of ambient particles under the severe biomass burning impact during haze events (Betha et al, 2014;Niu et al, 2016). Figure 4 shows the chemical evolution of aerosol particles during the 5 h photochemical aging of wheat straw burning.…”
Section: Evolution Of Particlessupporting
confidence: 65%
“…It is well established that particle size and chemical composition are key parameters that determine the health effects of PM [16][17][18][19]. Previous studies have reported that ultrafine particles (UFPs) (PM with aerodynamic diameter (AED) ≤100 nm) are prevalent during haze episodes [20][21][22][23][24]48]. However, there is a lack of research on these harmful and easily inhalable sub-micrometer particles in SEA.…”
Section: Introductionmentioning
confidence: 99%
“…Nevertheless, the effectiveness of these devices in reducing human exposure and the associated potential health risks based on the toxic elemental composition of PM indoors remains largely unknown. Additionally, previous studies reported in the literature [35,41] have been carried out under mid-latitude environmental conditions and thus are not applicable to tropical climatic conditions in SEA, where the smokehaze-impacted PM has unique physico-chemical characteristics [4,5,21,25].…”
Section: Introductionmentioning
confidence: 99%
“…Most of the researches have shown that both local rush hour traffic emission and new particle formation (NPF) play key roles in the diurnal variation of UFPs concentrations, in which two concentration peaks in the morning and evening could be attributed to traffic emission, while one peak in the afternoon is due to NPF (Young et al, 2012;Cheung et al, 2013;Young et al, 2013;Betha et al, 2014;Nikolova et al, 2014).…”
Section: Introductionmentioning
confidence: 99%
“…In the past, numerous studies used the Fast Mobility Particle Sizer (FMPS) (Westerdahl et al, 2009;Sabaliauskas et al, 2012;Betha et al, 2014;Kim et al, 2015) or the Scanning Mobility Particle Sizer (SMPS) coupled with the condensation particle counter (CPC) (Chen et al, 2010a;Breitner et al, 2011;Jayaratne et al, 2011;Wang et al, 2011;Xu et al, 2011;Gao et al, 2012;Young et al, 2012;Cheung et al, 2013;Young et al, 2013;Cheng et al, 2014) to investigate the number concentrations of UFPs. Most of the researches have shown that both local rush hour traffic emission and new particle formation (NPF) play key roles in the diurnal variation of UFPs concentrations, in which two concentration peaks in the morning and evening could be attributed to traffic emission, while one peak in the afternoon is due to NPF (Young et al, 2012;Cheung et al, 2013;Young et al, 2013;Betha et al, 2014;Nikolova et al, 2014).…”
Section: Introductionmentioning
confidence: 99%