Low hygroscopicity of ambient fresh carbonaceous aerosols from pyrotechnics smoke

Journal Article · Tue Jan 30 23:00:00 EST 2018 · Atmospheric Environment (1994)

DOI: https://doi.org/10.1016/j.atmosenv.2018.01.024 · OSTI ID:1419756

Carrico, Christian M.  ^[1]; Gomez, Samantha Laray ^[2]; Dubey, Manvendra Krishna  ^[3]; Aiken, Allison C.  ^[3]

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1. New Mexico Institute of Mining and Technology, Socorro, NM (United States)
2. New Mexico Institute of Mining and Technology, Socorro, NM (United States); Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
3. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

Pyrotechnics (fireworks) displays are common for many cultures worldwide, with Independence Day celebrations occurring annually on July 4th as the most notable in the U.S. Given an episodic nature, fireworks aerosol properties are poorly characterized. Here we report observations of optical properties of fresh smoke emissions from Independence Day fireworks smoke sampled at Los Alamos National Laboratory, New Mexico U.S.A. on 4–5 July 2016. Aerosol optical properties were measured with a photoacoustic extinctiometer (PAX, DMT, Inc., Model 870 nm) at low RH < 30% and a humidity controlled nephelometry system (Ecotech, Inc., 450 nm Aurora). ‘Dry’ light scattering coefficient (σsp) increased from background < 15 Mm^–1 reaching 120 Mm^–1 (450 nm) as a 2-min event peak, while the absorption coefficient increased from background of 0.5–4.4 Mm^–1 (870 nm). The event peak occurred at 00:35 on 5 July 2016, ~3 h after local fireworks events, and decreased to background by 04:00 on 5 July 2016, showing well mixed aerosol properties. A notable result is that the aerosol hygroscopic response, as characterized by the ratio of wet to dry light scattering or f(RH = 85%), declined to 1.02 at the peak fireworks influence from a background ~1.7. Strong wavelength dependence of light scattering with Ångström exponent ~2.2 throughout the event showed a size distribution dominated by sub-micrometer particles. Likewise, single scattering albedo at 870 nm remained constant throughout the event with ω = 0.86 ± 0.03, indicating light absorbing carbon, though not dominant, was mixed with organic carbon. Subsequent laboratory testing with ground-level sparklers showed that pyrotechnics smoke can generate a strong hygroscopic response, however. As confirmed with chemical analysis, the chemistry of the fireworks was key to defining the hygroscopic response. As a result, sparkler smoke was dominated by salt species such as hygroscopic potassium chloride while it lacked the black powder explosives in aerial fireworks that contribute organic and elemental carbon to its non-hygroscopic smoke.

• Research Organization: Los Alamos National Laboratory (LANL)
• Sponsoring Organization: USDOE Office of Science (SC), Workforce Development for Teachers and Scientists (WDTS) (SC-27); USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)
• Grant/Contract Number: AC52-06NA25396
• OSTI ID: 1419756
• Report Number(s): LA-UR-17-25199
• Journal Information: Atmospheric Environment (1994), Journal Name: Atmospheric Environment (1994) Journal Issue: C Vol. 178; ISSN 1352-2310
• Publisher: ElsevierCopyright Statement
• Country of Publication: United States
• Language: English