2021
DOI: 10.1016/j.atmosres.2021.105740
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Road dust resuspension: A review

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Cited by 74 publications
(31 citation statements)
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“…Road dust consists of particles present on the road surface, generated by traffic or transported and deposited from near or long-range sources. Brake wear particles, RWP and TRWP originating from road and traffic, are major components of road dust, , but winter traction sanding, building sites, wind-blown dust from bare soils, and dust dragged in by traffic from connecting unbound roads can be strong local sources. Source heterogeneity is reflected in the chemical composition (a mix of minerals, metals, and organic compounds) often occurring as aggregates with a high temporal and spatial variability.…”
Section: Emission Characteristics and Quantificationmentioning
confidence: 99%
See 1 more Smart Citation
“…Road dust consists of particles present on the road surface, generated by traffic or transported and deposited from near or long-range sources. Brake wear particles, RWP and TRWP originating from road and traffic, are major components of road dust, , but winter traction sanding, building sites, wind-blown dust from bare soils, and dust dragged in by traffic from connecting unbound roads can be strong local sources. Source heterogeneity is reflected in the chemical composition (a mix of minerals, metals, and organic compounds) often occurring as aggregates with a high temporal and spatial variability.…”
Section: Emission Characteristics and Quantificationmentioning
confidence: 99%
“…PM 10 EFs for resuspension on paved roads have been estimated using derivations from dust load, mobile measurements and vertical profile methods. Factors range from a few to ∼1000 mg·km –1 ·veh –1 for LDV and 150–8000 mg·km –1 ·veh –1 for HDV (using USEPA method based on silt loading and vertical profile of dust loading). PM 10 resuspension was between 13 and 32 mg·km –1 ·veh –1 for 10 sites in Milan, Italy .…”
Section: Emission Characteristics and Quantificationmentioning
confidence: 99%
“…The relative larger amount of dust in Santiago is probably related to the size of the city (1.7 million inhabitants compared to 90,000 in Quillota and 10,000 in Los Caleos), consequently there is more traffic and more activities that can resuspend dust into the air. Several studies have found that when there is little rain, materials that were previously deposited on road surface can be more easily resuspended (Amato et al, 2009;Karanasiou et al, 2011;Rienda and Alves, 2021). In addition Earlier work in Santiago has characterized the elemental composition of PM 10 and PM 2.5 with XRF.…”
Section: Chemical Speciationmentioning
confidence: 99%
“…However, there are several caveats to this conclusion: first, we use the steady-state γ BET value here, which underestimates the reactivity of road dust at shorter ozone exposure times; second, since the composition of road dust varies with both season ( e.g. , via loss of water-soluble material during spring melt and/or changes in contributions of individual components) and location, 109 ozone uptake by road dust may also vary. Nonetheless, as road dust mass loadings are typically orders of magnitude lower than this value, 110 we conclude that suspended road dust is not reactive enough to influence ozone mixing ratios in the urban atmosphere.…”
Section: Atmospheric Significance and Conclusionmentioning
confidence: 99%