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dc.contributor.authorDoerr, SH
dc.contributor.authorSantín, C
dc.contributor.authorMerino, A
dc.contributor.authorBelcher, CM
dc.contributor.authorBaxter, G
dc.date.accessioned2019-07-26T09:25:35Z
dc.date.issued2018-10-10
dc.description.abstractPyrogenic carbon (PyC, charcoal) is produced during vegetation fires at a rate of ~116–385 Tg C yr −1 globally. It represents one of the most degradation-resistant organic carbon pools, but its long-term fate and the processes leading to its degradation remain subject of debate. A frequently highlighted potential loss mechanism of PyC is its consumption in subsequent fires. However, only three studies to date have tested this hypothesis with reported losses of <8–37%, with the effects of PyC chemical characteristics and fire conditions on PyC loss in wildfires remaining unexplored. To address this, we placed materials with different degrees of thermal and chemical recalcitrance (A: wildfire charcoal, B: slash-pile charcoal, C: pine wood and D: cedar wood) on the ground surface just prior to a high-intensity and a low-intensity boreal forest wildfire. Mass losses were highly variable and dependent on fire- and sample characteristics. Mass losses across both fires (as % of dry weight) were for A: 66.5 ± 25.2, B: 41.7 ± 27.2, C: 78.2 ± 14.9, and D: 83.8 ± 18.9. Mass loss correlated significantly with maximum temperature (T max ) recorded on sample surfaces (r = 0.65, p = 0.01), but only weakly (r = 0.33) with time >300°C. Mass losses also showed a significant negative correlation (r = −0.38, p = 0.05) with thermal recalcitrance (T50) determined using Differential Scanning Calorimetry (DSC) and T max with charcoal reflectance (Ro) determined after the fires (r = 0.46, p = 0.05). Losses in the high-intensity fire were significantly higher (p = 0.05) than in the low-intensity fire, but the latter had a higher rate of conversion of fuel to PyC. Our results demonstrate that exposure to fire can indeed be a significant removal mechanism for PyC that remains exposed on the ground after a previous fire. The losses found, however, are likely to represent an extreme upper range as most PyC produced in a fire would not remain exposed on the ground surface by the time the next fire occurs. Our data also demonstrate, for real wildfire conditions, the (i) contrasting resistance of different PyC types to combustion and (ii) contrasting net PyC losses between different fire intensities. The DSC and reflectance (Ro) results support the usefulness of these analyses in reflecting thermal degradation resistance and temperature exposure under actual wildfire conditions.en_GB
dc.description.sponsorshipLeverhulme Trusten_GB
dc.description.sponsorshipEuropean Research Councilen_GB
dc.description.sponsorshipEuropean Union Horizon 2020en_GB
dc.identifier.citationVol. 6, article 127en_GB
dc.identifier.doi10.3389/feart.2018.00127
dc.identifier.grantnumberRPG-2014-095en_GB
dc.identifier.grantnumberRF-2016-456\2en_GB
dc.identifier.grantnumberERC-2013-StG-335891-ECOFLAMen_GB
dc.identifier.grantnumber663830en_GB
dc.identifier.urihttp://hdl.handle.net/10871/38118
dc.language.isoenen_GB
dc.publisherFrontiers Mediaen_GB
dc.rights© 2018 Doerr, Santín, Merino, Belcher and Baxter. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.en_GB
dc.subjectblack carbonen_GB
dc.subjectboreal foresten_GB
dc.subjectcarbon balanceen_GB
dc.subjectcharcoalen_GB
dc.subjectcharcoal reflectanceen_GB
dc.subjectwildfireen_GB
dc.subjectmanagement burnen_GB
dc.subjectthermal analysisen_GB
dc.titleFire as a Removal Mechanism of Pyrogenic Carbon From the Environment: Effects of Fire and Pyrogenic Carbon Characteristicsen_GB
dc.typeArticleen_GB
dc.date.available2019-07-26T09:25:35Z
dc.descriptionThis is the final version. Available on open access from Frontiers Media via the DOI in this recorden_GB
dc.identifier.eissn2296-6463
dc.identifier.journalFrontiers in Earth Scienceen_GB
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2018-08-10
exeter.funder::European Commissionen_GB
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2018-10-10
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2019-07-26T09:22:30Z
refterms.versionFCDVoR
refterms.dateFOA2019-07-26T09:25:38Z
refterms.panelCen_GB
refterms.depositExceptionpublishedGoldOA


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© 2018 Doerr, Santín, Merino, Belcher and Baxter. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
Except where otherwise noted, this item's licence is described as © 2018 Doerr, Santín, Merino, Belcher and Baxter. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.