Taking advantage of only the measured aerosol particles spectral evolution
as a function of time, a new analytical tool is developed to derive formati
on and growth properties of nucleation mode aerosols. This method, when use
d with hygroscopic growth-factors, can also estimate basic composition prop
erties of these recently-formed particles. From size spectra the diameter g
rowth-rate can be obtained, and aerosol condensation and coagulation sinks
can be calculated. Using this growth-rate and condensation sink, the concen
tration of condensable vapours and their source rate can be estimated. Then
, combining the coagulation sink together with measured number concentratio
ns and apparent source rates of 3 run particles, I nm particle nucleation r
ates and concentration can be estimated. To estimate nucleation rates and v
apour concentration source rates producing new particle bursts over the Bor
eal forest regions, three cases from the BIOFOR project were examined using
this analytical tool. In this environment, the nucleation mode growth-rate
was observed to be 2-3 nm hour(-1), which required a condensable vapour co
ncentration of 2.5-4 x 10(7) cm(-3) and a source rate of approximately 7.5-
11 x 10(4) cm(-3) s(-1) to be sustained. The formation rate of 3 nm particl
es was approximate to 1 particle cm(-)3 s(-1) in all three cases. The estim
ated formation rate of 1 nm particles was 10-100 particles cm(-3) s(-1), wh
ile their concentration was estimated to be between 10,000 and 100,000 part
icles cm(-3). Using hygroscopicity data and mass flux expressions, the mass
flux of insoluble vapour is estimated to be of the same order of magnitude
as that of soluble vapour, with a soluble to insoluble vapour flux ratio r
anging from 0.7 to 1.4 during these nucleation events.