Chemically distinct particle-phase emissions from highly controlled pyrolysis of three wood types
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Published:2023-08-09
Issue:15
Volume:23
Page:8837-8854
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Avery Anita M.ORCID, Fawaz Mariam, Williams Leah R., Bond TamiORCID, Onasch Timothy B.ORCID
Abstract
Abstract. Wood pyrolysis is a distinct process that precedes
combustion and contributes to biomass and biofuel burning gas-phase and
particle-phase emissions. Pyrolysis is defined as the thermochemical
degradation of wood, the products of which can be released directly or
undergo further reaction during gas-phase combustion. To isolate and study
the processes and emissions of pyrolysis, a custom-made reactor was used to
uniformly heat small blocks of wood in a nitrogen atmosphere. Pieces of
maple, Douglas fir, and oak wood (maximum of 155 cm3) were pyrolyzed in a
temperature-controlled chamber set to 400, 500, or 600 ∘C. Real-time particle-phase emissions were measured with a soot particle aerosol
mass spectrometer (SP-AMS) and correlated with simultaneous gas-phase
emission measurements of CO. Particle and gas emissions increased rapidly
after inserting a wood sample, remained high for tens of minutes, and then
dropped rapidly leaving behind char. The particulate mass-loading profiles
varied with elapsed experiment time, wood type and size, and pyrolysis
chamber temperature. The chemical composition of the emitted particles was
organic (C, H, O), with negligible black carbon or nitrogen. The emitted
particles displayed chemical signatures unique to pyrolysis and were notably
different from flaming or smoldering wood combustion. The most abundant
fragment ions in the mass spectrum were CO+ and CHO+, which
together made up 23 % of the total aerosol mass on average, whereas
CO2+ accounted for less than 4 %, in sharp contrast with ambient
aerosol where CO2+ is often a dominant contributor. The mass
spectra also showed signatures of levoglucosan and other anhydrous sugars.
The fractional contribution of m/z 60, traditionally a tracer for anhydrous
sugars including levoglucosan, to total loading (f60) was observed to be
between 0.002 and 0.039, similar to previous observations from wildfires and
controlled wood fires. Atomic ratios of oxygen and hydrogen to carbon, O:C
and H:C as calculated from AMS mass spectra, varied between 0.41–0.81 and
1.06–1.57, respectively, with individual conditions lying within a continuum
of O:C and H:C for wood's primary constituents: cellulose, hemicellulose,
and lignin. This work identifies the mass spectral signatures of particle
emissions directly from pyrolysis, including f60 and
the CO+/CO2+ ratio, through controlled laboratory experiments in
order to help in understanding the importance of pyrolysis emissions in the
broader context of wildfires and controlled wood fires.
Funder
Division of Atmospheric and Geospace Sciences
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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