Data from: Chemically distinct particle phase emissions from highly controlled pyrolysis of three wood types
Data files
Jul 02, 2023 version files 174.46 KB
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Figure1a.csv
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Figure1b.csv
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Figure1c.csv
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Figure2.csv
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Figure3_VanKrevelen.csv
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Figure4a.csv
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Figure4b.csv
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Figure4c.csv
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Figure4d.csv
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Figure5_multipanel.csv
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Figure6.csv
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Figure7.csv
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Figure8.csv
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FigureS1.csv
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FigureS2.csv
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FigureS3.csv
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README.MD
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 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 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 wild 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 CO+/CO2+ ratio, through controlled laboratory experiments in order to help understand the importance of pyrolysis emissions in the broader context of wild and controlled wood fires.
Methods
In each experiment, individual pieces of wood were heated under N2 so as to measure the pyrolysis products primarily with an Aerosol Mass Spectrometer (AMS). The emissions from pyrolysis were entirely organic and further analyzed by individual ion fragments and bulk properties including O/C, H/C, and oxidation state.
This dataset includes the total organic, individual ion, and O/C and H/C ratio data obtained with the AMS, along with the mass loss and gas phase measurements that comprise the figures in this paper.
This data was processed into its current form from raw data using the openly accessible Squirrel and Pika software for AMS data, including calculation of O/C and H/C ratios from individually fit ion fragments. The software can be found at: https://cires1.colorado.edu/jimenez-group/ToFAMSResources/ToFSoftware/
Usage notes
Data from each figure are provided as csv files.