Abstract
The rates of formation of aerosols and the visual appearance of chimney plumes (including the effects of condensation of water vapour) both depend upon the dilution of the effluent gases. This dilution differs from that predicted by conventional dispersion formulae in that these latter refer to time mean concentrations, whereas what is required is the dilution at any given instant in time as the plume travels downwind.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have