Abstract

Dispersion of chemically reactive pollutants in the urban canopy layer (UCL) over twelve idealised two-dimensional (2D) street canyons of unity aspect ratio in isothermal conditions is examined. The reversible NO x -O 3 mechanism is integrated into a large-eddy simulation (LES) model. The ground-level NO emission in the first street canyon and the background O 3 in the prevailing wind initiate the NO 2 production. The chemical equilibrium is measured by the photostationary state (PSS) which is a function of the time scales of turbulent mixing and chemical reactions. PSS of the first street canyon increases with increasing NO emission. For small amount of ground-level NO emission and background O 3 in the prevailing flows, (say NO/O 3 = 1/1), PSS increases gradually from the second to last street canyons. It increases faster if the NO-to-O 3 ratio is raised, say 1,000/30. Further increasing the NO-to-O 3 ratio, say 10,000/1, PSS exhibits a non-linear behaviour in which a trough is observed in the fifth street canyon.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.