“…Atmospheric gases such as NO x (NO 2 and NO) are produced outdoors through the combustion of fossil fuels and are present in urban atmospheres at or up to several hundred parts per billion by volume. − Reactions involving NO x and VOCs are responsible for the production of tropospheric ozone (O 3 ); furthermore, NO x is a precursor to HONO, which is a photochemical source of OH radicals under illumination conditions where O 3 chemistry is not important. , Overall, NO x is partially responsible for urban smog, as well as acid rain and other pollution events harmful to human health . Dirty city surfaces are known to be effective at recycling NO x ; , for example, Baergen and Donaldson showed that heterogeneous photochemistry of nitrate anions present in the film of atmospheric constituents deposited onto urban surfaces (known as urban grime) produces NO x and other reactive species. Photochemical, humidity-dependent uptake of NO 2 onto urban grime has also been reported as a significant source of HONO, which could affect the oxidative capacity of the daytime urban atmosphere. , In addition, NO x reacts heterogeneously with mineral dust, , a major component of road dust. , In this reaction, NO 2 first adsorbs to the surface of the dust, then produces gas-phase NO and nitrate. , Finally, road dust itself has recently been shown to be photochemically active; it can produce singlet oxygen upon illumination when in aqueous suspended state, which suggests the potential for heterogeneous photochemistry.…”