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Download fileCompositional Characterization of Phase-Separated Pine Wood Slow Pyrolysis Oil by Negative-Ion Electrospray Ionization Fourier Transform Ion Cyclotron Resonance Mass Spectrometry
journal contribution
posted on 2015-12-17, 07:40 authored by Ilja Miettinen, Marko Mäkinen, Teemu Vilppo, Janne JänisThe chemical composition of slow
pyrolysis oil made from unbarked
Scots pine (Pinus sylvestris) was characterized by
negative-ion electrospray ionization Fourier transform ion cyclotron
resonance (ESI FT-ICR) mass spectrometry and various bulk analyses.
The wood pieces were heated stepwise in a batch pyrolysis reactor
to the target temperature of 320 °C. The resulting pyrolysis
oil spontaneously separated into aqueous and oily phases. The water
content of the aqueous phase was as high as 60.4 wt %, whereas for
the oily phase it was only 8.1 wt %. The bulk O/C ratio (on a dry
basis) was more than twice as high for the aqueous phase as compared
to the oily phase (0.61 vs 0.29), suggesting different chemistry between
the two phases. On the basis of pH and total acid number measurements,
the aqueous phase was more acidic than the oily phase. The ESI FT-ICR
technique was used to characterize pyrolysis oils’ heavier,
nonvolatile, and thermally labile species. The total amounts of the
identified chemical formulas were ∼540 and ∼630 for
the aqueous and oily phases, respectively. The majority of the detected
compounds were oxygen-containing species, representing heteroatom
classes O2–O14. The O9–O14 class compounds were present only in the aqueous phase.
The O2–O4 compounds were comprised of
different acids, including resin acids and several types of fatty
acids, such as hydroxy fatty acids and diacids, which were concentrated
in the oily phase. However, saturated fatty acids were more dominant
in the aqueous phase, possibly due to their increased solubility through
micelle formation in a more aqueous environment. Anhydrosugars and
other high oxygen-containing compounds were present only in the aqueous
phase. Both phases also contained condensed aromatic compounds (pyrolytic
lignin), representing heteroatom classes O3–O8.