Perchlorate behavior in the context of black carbon and metal cogeneration following fireworks emission at Oak Lake, Lincoln, Nebraska, USA

• Published in: Environmental pollution (1987) Vol. 253; pp. 930 - 938
• Main Authors: Kumar, Manish, Snow, Daniel D., Li, Yusong, Shea, Patrick J.
• Format: Journal Article
• Language: English
• Published: England Elsevier Ltd 01.10.2019
• Subjects: Black carbon; Cogeneration; Fireworks; Lake water system; Metal; Perchlorate; Perchlorate; Metal; Cogeneration; Black carbon; Fireworks; Lake water system
• ISSN: 0269-7491; 1873-6424
• DOI: 10.1016/j.envpol.2019.07.038

The imprints of fireworks displays on the adjacent water body were investigated from the perspective of cogeneration of black carbon, metals and perchlorate (ClO4−). In particular, the mixing and dissipation of ClO4− were studied at Oak Lake, Lincoln, Nebraska, following fireworks displays in 2015 and 2016. Following the display, ClO4− concentration in the water increased up to 4.3 μg/L and 4.0 μg/L in 2015 and 2016, respectively. A first-order model generally provided a good fit to the measured perchlorate concentrations from which the rate of dissipation was estimated as 0.07 d−1 in 2015 and 0.43 d−1 in 2016. SEM images show imprints of soot and metal particles in aerosol samples. EDS analysis of the lake sediment confirmed the presence of Si, K, Ca, Zn and Ba, most of which are components of fireworks. The δ13C range of −7.55‰ to −9.19‰ in the lake water system closely resembles fire-generated carbon. Cogeneration of black carbon and metal with perchlorate was established, indicating that ClO4− is an excellent marker of fireworks or a burning event over all other analyzed parameters. Future microcosmic, aggregation and column-based transport studies on black carbon in the presence of perchlorate and metals under different environmental conditions will help in developing transport and fate models for perchlorate and black carbon particles. [Display omitted] •A fireworks display cogenerated black carbon, metal and perchlorate (ClO4−).•ClO4− in adjacent lake water increased up to 4.3 μg/L after the fireworks.•ClO4− dissipation rate constants were 0.07 d−1 in 2015 and 0.43 d−1 in 2016.•A δ13C range of −7.55‰ to −9.19‰ in lake water resembles fire-generated carbon.•Findings indicate ClO4− is an excellent marker of fireworks or a burning event. Black carbon, metal and perchlorate are cogenerated from fireworks display followed by perchlorate dissipation through dilution and pseudo first-order decay.