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

被引:0
作者
Baalousha, Mohammed [1 ]
Desmau, Morgane [2 ]
Singerling, Sheryl A. [3 ]
Webster, Jackson P. [4 ]
Matiasek, Sandrine J. [5 ]
Stern, Michelle A. [6 ]
Alpers, Charles N. [6 ]
机构
[1] Univ South Carolina, Ctr Environm Nanosci & Risk, Arnold Sch Publ Hlth, Dept Environm Hlth Sci, Columbia, SC 29208 USA
[2] Deutsch Elektronen Synchrotron DESY, Notkestr 85, D-22607 Hamburg, Germany
[3] Virginia Polytech Inst & State Univ, Natl Ctr Earth & Environm Nanotechnol Infrastruct, Inst Crit Technol & Appl Sci, Blacksburg, VA 24061 USA
[4] Calif State Univ Chico, Dept Civil Engn, 400 W 1st St, Chico, CA 95929 USA
[5] Calif State Univ Chico, Dept Earth & Environm Sci, 400 W 1st St, Chico, CA 95929 USA
[6] US Geol Survey, Calif Water Sci Ctr, 6000 J St, Sacramento, CA 95819 USA
基金
美国国家科学基金会;
关键词
PARTICULATE MATTER; AIR-POLLUTION; REDUCTION; SPECIATION; HEMATITE; TRANSFORMATION; ABSORPTION; WILDFIRE; MAGNETIZATION; LEPIDOCROCITE;
D O I
10.1039/d2en00439a
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
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.
引用
收藏
页码:4136 / 4149
页数:15
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