A systematic comparison of spectra obtained with extra and in situ diagnost
ics in the soot preinception region of rich, premixed ethylene air flames s
uggests that combustion generated organic carbon (OC) particulate can be ex
tracted from flames and isolated from other flame material for further chem
ical analysis. Both the trend with height above the burner and the form of
UV fluorescence and absorption spectra from extra situ sampled material cap
tured in water agree with those measured in situ. These results show that t
he OC particulate formed in flames is partially water soluble. However, the
collection efficiency can be increased using less polar solvents, like ace
tonitrile and dichloromethane. The fluorescence spectra from the water samp
les are comprised both a naphthalene-like component and a broad band UV flu
orescence component similar to that observed in situ which is attributed to
flame generated OC particulate. The broad band UV fluorescence centered ar
ound 320 nm is also observed very early in flames and does not change consi
derably with increasing flame residence time. These results support previou
s hypotheses that the UV broad band fluorescence is from carbonaceous mater
ial comprised two-ring aromatics, formed earlier than soot in the flame, an
d is still present along with soot at higher heights or flame residence tim
es. (C) 2001 Elsevier Science Ltd. All rights reserved.