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Open AccessJournal ArticleDOI

Physical characterization of aerosol particles during nucleation events

TLDR
Particle concentrations and size distributions have been measured from different heights inside and above a boreal forest during three BIOFOR campaigns (14 April-22 May 1998, 27 July-21 August 1998 and 20 March-24 April 1999) in Hyytiala, Finland.
Abstract
Particle concentrations and size distributions have been measured from different heights inside and above a boreal forest during three BIOFOR campaigns (14 April–22 May 1998, 27 July–21 August 1998 and 20 March–24 April 1999) in Hyytiala, Finland Typically, the shape of the background distribution inside the forest exhibited 2 dominant modes: a fine or Aitken mode with a geometric number mean diameter of 44 nm and a mean concentration of 1160 cm −3 and an accumulation mode with mean diameter of 154 nm and a mean concentration of 830 cm −3 A coarse mode was also present, extending up to sizes of 20 μm having a number concentration of 12 cm −3 , volume mean diameter of 20 μm and a geometric standard deviation of 19 Aerosol humidity was lower than 50% during the measurements Particle production was observed on many days, typically occurring in the late morning Under these periods of new particle production, a nucleation mode was observed to form at diameter of the order of 3 nm and, on most occasions, this mode was observed to grow into Aitken mode sizes over the course of a day Total concentrations ranged from 410–45 000 cm −3 , the highest concentrations occurring on particle production days A clear gradient was observed between particle concentrations encountered below the forest canopy and those above, with significantly lower concentrations occurring within the canopy Above the canopy, a slight gradient was observed between 18 m and 67 m, with at maximum 5% higher concentration observed at 67 m during the strongest concentration increases DOI: 101034/j1600-08892001530403x

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Citations
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Journal ArticleDOI

Formation and growth rates of ultrafine atmospheric particles: a review of observations

TL;DR: In this paper, the formation rate of 3-nm particles is often in the range 0.01-10 cm −3 s −1 in the boundary layer in urban areas and in coastal areas and industrial plumes.
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Formation of Urban Fine Particulate Matter

TL;DR: Air pollutants consist of a complex combination of gases and particulate matter, which is emitted directly into the atmosphere or formed in the atmosphere through gas-to-particle conversion (secondary) (Figure 1).
Journal ArticleDOI

Nucleation and Growth of Nanoparticles in the Atmosphere

TL;DR: Nucleation and Growth of Nanoparticles in the Atmosphere Renyi Zhang,* Alexei Khalizov, Lin Wang, Min Hu, and Wen Xu.
Journal Article

Formation and growth of fresh atmospheric aerosols: eight years of aerosol size distribution data from SMEAR II, Hyytiälä, Finland

TL;DR: In this paper, the authors analyzed size distributions measured continuously at a boreal forest measurement site at Hyytiala, Finland between 1996 and 2003 and identified days when new aerosol particle formation was taking place as well as days when no formation was detected, removing days with ambiguous status.
Journal ArticleDOI

On the formation, growth and composition of nucleation mode particles

TL;DR: In this article, a new analytical tool was developed to derive formation and growth properties of nucleation mode aerosols, taking advantage of only the measured aerosol particles spectral evolution as a function of time.
References
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Journal ArticleDOI

A new electromobility spectrometer for the measurement of aerosol size distributions in the size range from 1 to 1000 nm

TL;DR: The Electromobility Spectrometer as mentioned in this paper is an automated measurement system for the size analysis of fine and ultrafine aerosols using Differential Mobility Analysers (DMA) for the classification of particles and an electrical sensor for their detection.
Journal ArticleDOI

An Ultrafine Aerosol Condensation Nucleus Counter

TL;DR: In this paper, a condensation nucleus counter (CNC) for detecting ultrafine aerosol (UFA) particles (particle diameter ≤ 20 nm) is described, which is designed specifically for high-efficiency detection and counting of ultrafine particles.
Journal ArticleDOI

Observations of ultrafine aerosol particle formation and growth in boreal forest

TL;DR: In this article, the number size distribution of ambient submicron and ultrafine aerosol particles have been measured on a continuous basis (every 10 minutes) for three quarters of the year 1996, at a forest site in Southern Finland.
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