4.6 Article

Discovery and potential ramifications of reduced iron-bearing nanoparticles-magnetite, wustite, and zero-valent iron-in wildland-urban interface fire ashes

Journal

ENVIRONMENTAL SCIENCE-NANO
Volume 9, Issue 11, Pages 4136-4149

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/d2en00439a

Keywords

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Funding

  1. RAPID grant from United States National Science Foundation (NSF) [2101983]
  2. Nanoscale Characterization and Fabrication Laboratory
  3. Virginia Tech National Center for Earth and Environmental Nanotechnology Infrastructure (NanoEarth) - NSF [ECCS 1542100, ECCS 2025151]
  4. Div Of Chem, Bioeng, Env, & Transp Sys
  5. Directorate For Engineering [2101983] Funding Source: National Science Foundation

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The presence of iron-bearing nanoparticles in ash after wildland-urban interface fires and their varying concentrations and species composition have been investigated, showing the impact of fires on iron speciation. The concentration of magnetite nanoparticles decreases with the color of the ash.
The increase in fires at the wildland-urban interface has raised concerns about the potential environmental impact of ash remaining after burning. Here, we examined the concentrations and speciation of iron-bearing nanoparticles in wildland-urban interface ash. Total iron concentrations in ash varied between 4 and 66 mg g(-1). Synchrotron X-ray absorption near-edge structure (XANES) spectroscopy of bulk ash samples was used to quantify the relative abundance of major Fe phases, which were corroborated by transmission electron microscopy measurements. Maghemite (gamma-(Fe3+)(2)O-3) and magnetite (gamma-Fe2+(Fe3+)(2)O-4) were detected in most ashes and accounted for 0-90 and 0-81% of the spectral weight, respectively. Ferrihydrite (amorphous Fe(iii)-hydroxide, (Fe3+)(5)HO8 center dot 4H(2)O), goethite (alpha-Fe3+OOH), and hematite (alpha-Fe23+O3) were identified less frequently in ashes than maghemite and magnetite and accounted for 0-65, 0-54, and 0-50% of spectral weight, respectively. Other iron phases identified in ashes include wustite (Fe2+O), zerovalent iron, FeS, FeCl2, FeCl3, FeSO4, Fe-2(SO4)(3), and Fe(NO3)(3). Our findings demonstrate the impact of fires at the wildland-urban interface on iron speciation; that is, fires can convert iron oxides (e.g., maghemite, hematite, and goethite) to reduced iron phases such as magnetite, wustite, and zerovalent iron. Magnetite concentrations (e.g., up to 25 mg g(-1)) decreased from black to gray to white ashes. Based on transmission electron microscopy (TEM) analyses, most of the magnetite nanoparticles were less than 500 nm in size, although larger particles were identified. Magnetite nanoparticles have been linked to neurodegenerative diseases as well as climate change. This study provides important information for understanding the potential environmental impacts of fires at the wildland-urban interface, which are currently poorly understood.

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