Size fractionation as a tool for separating charcoal of different fuel source and recalcitrance in the wildfire ash layer.

Sci Total Environ

Dipartimento di Scienze delle Produzioni Agroalimentari e dell'Ambiente (DISPAA), Università degli Studi di Firenze, Piazzale delle Cascine 28, 50144 Firenze, Italy.

Published: October 2017

AI Article Synopsis

  • Charcoal's varied properties complicate studies on its role in reconstructing wildfire histories, leading researchers to explore the significance of particle size in categorizing combustion products.
  • The study analyzed ash/charcoal from different severity wildfires in Australia and Italy, fractionating samples into four sizes and assessing their chemical characteristics, composition, and structure.
  • Findings indicated that finer charcoal particles contained less carbon and higher mineral ash, while coarser fractions retained more amorphous carbon, suggesting that particle size affects the properties of charcoal based on fuel type and burning conditions.

Article Abstract

Charcoal is a heterogeneous material exhibiting a diverse range of properties. This variability represents a serious challenge in studies that use the properties of natural charcoal for reconstructing wildfires history in terrestrial ecosystems. In this study, we tested the hypothesis that particle size is a sufficiently robust indicator for separating forest wildfire combustion products into fractions with distinct properties. For this purpose, we examined two different forest environments affected by contrasting wildfires in terms of severity: an eucalypt forest in Australia, which experienced an extremely severe wildfire, and a Mediterranean pine forest in Italy, which burned to moderate severity. We fractionated the ash/charcoal layers collected on the ground into four size fractions (>2, 2-1, 1-0.5, <0.5mm) and analysed them for mineral ash content, elemental composition, chemical structure (by IR spectroscopy), fuel source and charcoal reflectance (by reflected-light microscopy), and chemical/thermal recalcitrance (by chemical and thermal oxidation). At both sites, the finest fraction (<0.5mm) had, by far, the greatest mass. The C concentration and C/N ratio decreased with decreasing size fraction, while pH and the mineral ash content followed the opposite trend. The coarser fractions showed higher contribution of amorphous carbon and stronger recalcitrance. We also observed that certain fuel types were preferentially represented by particular size fractions. We conclude that the differences between ash/charcoal size fractions were most likely primarily imposed by fuel source and secondarily by burning conditions. Size fractionation can therefore serve as a valuable tool to characterise the forest wildfire combustion products, as each fraction displays a narrower range of properties than the whole sample. We propose the mineral ash content of the fractions as criterion for selecting the appropriate number of fractions to analyse.

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http://dx.doi.org/10.1016/j.scitotenv.2017.03.295DOI Listing

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