740
J. Kjallstrand et al. / Chemosphere 41 (2000) 735±741
rials, which were also burning in dierent ways. The
highest 2-methoxyphenol concentrations were observed
from pine bark and spruce twigs. The average amount of
methoxyphenols relative to CO was as high as 10% for
the softwood samples and even higher for the birchwood
sample. These amounts of methoxyphenols relative to
CO are at least 10 times higher than the amounts re-
ported for each of the major volatile organic compounds
methane, ethane, methanol, and acetic acid from
smouldering combustion of forest biomass (McKenzie
et al., 1995). They are also 10 times higher than the re-
corded methoxyphenol levels, evidently due to a low
recovery of these semivolatile compounds.
tions of gaseous methoxyphenols in ambient air are
biased towards the most volatile species.
4. Conclusions
The results demonstrate that methoxyphenols are
formed in high concentrations and speci®c proportions
from inecient biomass burning. Syringe sampling im-
mediately followed by GC±MS analysis permits
adequate determination of the methoxyphenols in lab-
oratory experiments. Adsorption on Tenax cartridges,
followed by thermal desorption, is an optional method
suitable also for ®eld sampling.
Approximately 1 kg of CO2 is formed from natural
burning of 1 kg of forest biomass (McKenzie et al.,
1995). From the results in Table 1 it is concluded that
the amount of released methoxyphenols was of the order
The reported smoke components are indicative of
emissions from accidental and planned forest ®res and
other inecient biomass burning. A major environ-
mental concern is the formation of ozone and other
photo-oxidants from gaseous smoke constituents. The
condensation of the methoxyphenols on particles de-
creases their contribution to ground-level ozone forma-
tion. Particles covered by adsorbed methoxyphenols and
anhydrosugars should also have very dierent health
eects compared with particles from trac and other
sources.
1
10 g kg of burnt biomass. Previously, the complex
mixture of volatile hydrocarbons has been studied for
biomass burning under similar conditions (Barrefors
and Petersson, 1995). The ratio of total non-methane
1
volatile hydrocarbons varied from 10
g
kg
for
1
smouldering, to 0.1 g kg for ¯aming combustion of
wood. Similarly increased emissions with decreased
combustion eciency have been reported for other
volatile compounds emitted from forest biomass burn-
ing (McKenzie et al., 1995). It is concluded that meth-
1
oxyphenol emissions markedly exceeding 10 g kg are
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