Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Size-resolved effective density of urban aerosols in Shanghai
Abstract Size-resolved effective density of 50–400 nm urban particles was determined by a TDMA–APM system in Shanghai during wintertime. The average effective density ranged from 1.36 to 1.55 g cm−3, increasing with the particle diameter. The size dependent increase of density was consistent with previous hygroscopic measurements. We attributed the increase in density to the condensation of hygroscopic secondary aerosols and large massive organics. The diurnal variation of effective density was pronounced for smaller particles. A similar diurnal pattern was observed between particle density and the contribution of secondary NH4NO3 and (NH4)2SO4 to PM1.0, suggesting that density change in response to particle compositions. The effective density of Aitken mode particles had a considerable increase during the NPF event, in agreement with the contribution of sulfate. Particle mass distribution was derived from particle number distribution in combination with effective density. PM0.6 was highly correlated with PM1.0, revealing that secondary aerosols tend to condense on smaller particles.
Highlights Effective density of atmospheric aerosols was measured online using DMA–APM system. Effective density increased considerably with increasing particle size. Density variation was highly correlated with the mass fraction of secondary inorganic aerosols. Aitken mode particles had a rapid increase in the effective density during a new particle formation event. Precipitation scavenging had significant impact on both particle mass loading and effective density distribution.
Size-resolved effective density of urban aerosols in Shanghai
Abstract Size-resolved effective density of 50–400 nm urban particles was determined by a TDMA–APM system in Shanghai during wintertime. The average effective density ranged from 1.36 to 1.55 g cm−3, increasing with the particle diameter. The size dependent increase of density was consistent with previous hygroscopic measurements. We attributed the increase in density to the condensation of hygroscopic secondary aerosols and large massive organics. The diurnal variation of effective density was pronounced for smaller particles. A similar diurnal pattern was observed between particle density and the contribution of secondary NH4NO3 and (NH4)2SO4 to PM1.0, suggesting that density change in response to particle compositions. The effective density of Aitken mode particles had a considerable increase during the NPF event, in agreement with the contribution of sulfate. Particle mass distribution was derived from particle number distribution in combination with effective density. PM0.6 was highly correlated with PM1.0, revealing that secondary aerosols tend to condense on smaller particles.
Highlights Effective density of atmospheric aerosols was measured online using DMA–APM system. Effective density increased considerably with increasing particle size. Density variation was highly correlated with the mass fraction of secondary inorganic aerosols. Aitken mode particles had a rapid increase in the effective density during a new particle formation event. Precipitation scavenging had significant impact on both particle mass loading and effective density distribution.
Size-resolved effective density of urban aerosols in Shanghai
Yin, Zi (Autor:in) / Ye, Xingnan (Autor:in) / Jiang, Shuqin (Autor:in) / Tao, Ye (Autor:in) / Shi, Yang (Autor:in) / Yang, Xin (Autor:in) / Chen, Jianmin (Autor:in)
Atmospheric Environment ; 100 ; 133-140
30.10.2014
8 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch