T. Hoffmann et al., MOLECULAR COMPOSITION OF ORGANIC AEROSOLS FORMED IN THE ALPHA-PINENE O-3 REACTION - IMPLICATIONS FOR NEW PARTICLE FORMATION PROCESSES/, J GEO RES-A, 103(D19), 1998, pp. 25569-25578
The molecular composition of particle phase ozonolysis products of alp
ha-pinene is investigated to comprehend the aerosol formation process
following the VOC oxidation, focusing on an understanding of new parti
cle formation. Two analytical approaches are applied to identify low-v
olatile oxidation products in the particle phase; off-line investigati
ons using preconcentration on Tenax TA(R) followed by solvent extracti
on and liquid chromatography/mass spectrometry as well as an on-line t
echnique, in which the organic aerosols are introduced directly into t
he ion source of a mass spectrometer (atmospheric pressure chemical io
nization/mass spectrometry (APCI/MS)). Both techniques showed the form
ation of difunctional carboxylic acids, compounds whose physico-chemic
al properties will govern most of their mass into the particle phase.
Furthermore, stable binary diacid adducts could be identified by MSn-e
xperiments. These observations might give insight into the process of
new particle formation by heteromolecular homogeneous nucleation, indi
cating that the initial cluster formation cannot be described by macro
scopic properties of single oxidation products. Instead, strong interm
olecular forces between different diacids might play a key role in the
formation of initial nuclei and their subsequent growth.