1. |
- Hirsikko, Anne, et al.
(author)
-
Indoor and outdoor air ions and aerosol particles in the urban atmosphere of Helsinki : characteristics, sources and formation
- 2007
-
In: Boreal environment research. - 1239-6095 .- 1797-2469. ; 12:3, s. 295-310
-
Journal article (peer-reviewed)abstract
- We measured air ion size distributions with an air ion spectrometer in the size range of 0.34-40.3 nm both indoors (in July) and outdoors (in August) in Helsinki, Finland in 2004. At the same time we measured particle number concentrations and size distributions with two condensation particle counters (indoors) and differential mobility particle sizer (outdoors). Our main focus was to study new-particle formation in an urban site. We observed new-particle formation indoors almost every day, even many times a day, and four times outdoors. Indoors, the observed growth rates were 2.3-4.9 nm h-' for 1.3-3-nm ions, 6.5-8.7 nm h(-1) for 3-7-nm ions and 5.1-8.7 nm h-' for 7-20-nm ions. Outdoor ions (3-7 nm) grew at rates as large as 15.4 nm h-'. Outdoor ion and particle number concentrations were dependent on the wind direction, whereas indoor concentrations were dependent on ventilation conditions. Secondary particle formation and growth affected concentrations both indoors and outdoors. We concluded, based on our measurement results and simulated penetration of outdoor particles through the ventilation system, that we had indoor sources for secondary particles.
|
|
2. |
- Svenningsson, Birgitta, et al.
(author)
-
Aerosol particle formation events and analysis of high growth rates observed above a subarctic wetland-forest mosaic
- 2008
-
In: Tellus. Series B: Chemical and Physical Meteorology. - : Stockholm University Press. - 0280-6509 .- 1600-0889. ; 60, s. 353-364
-
Journal article (pop. science, debate, etc.)abstract
- An analysis of particle formation (PF) events over a subarctic mire in northern Sweden was performed, based on number size distributions of atmospheric aerosol particles (10-500 nm in diameter) and ions (0.4-40 nm in Tammet diameter). We present classification statistics for PF events from measurements covering the period July 2005- September 2006, with a break over the winter period. The PF event frequency peaked during the summer months, in contrast to other Scandinavian sites where the frequency is highest during spring and autumn. Our analysis concentrates on calculated growth rates and estimates of concentrations and production rates of condensing vapour, deduced from the growth rates and condensational sink calculations, using AIS and SMPS data. Particle formation events with high growth rates (up to 50 nm/h) occurred repeatedly. In these cases, the newly formed nucleation mode particles were often only present for periods of a few hours. On several occasions repeated particle formation events were observed within one day, with differences in onset time of a few hour. These high growth rates were only observed when the condensation sink was higher than 0.001 s-1.
|
|