Title of article :
Effect of wind direction and speed on the dispersion of
nucleation and accumulation mode particles in an urban
street canyon
Author/Authors :
Prashant Kumara، نويسنده , , ?، نويسنده , , Paul Fennellb، نويسنده , , Rex Brittera، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2008
Abstract :
There have been many studies concerning dispersion of gaseous pollutants from vehicles
within street canyons; fewer address the dispersion of particulate matter, particularly
particle number concentrations separated into the nucleation (10–30 nm or N10–30) or
accumulation (30–300 nm or N30–300) modes either separately or together (N10–300).
This study aimed to determine the effect of wind direction and speed on particle dispersion
in the above size ranges. Particle number distributions (PNDs) and concentrations (PNCs)
were measured in the 5–2738 nm range continuously (and in real-time) for 17 days between
7th and 23rd March 2007 in a regular (aspect ratio~unity) street canyon in Cambridge (UK),
using a newly developed fast-response differential mobility spectrometer (sampling
frequency 0.5 Hz), at 1.60 m above the road level. The PNCs in each size range, during all
wind directions, were better described by a proposed two regime model (traffic-dependent
and wind-dependent mixing) than by simply assuming that the PNC was inversely
proportional to the wind speed or by fitting the data with a best-fit single power law. The
critical cut-off wind speed (Ur,crit) for each size range of particles, distinguishing the
boundary between these mixing regimes was also investigated. In the traffic-dependent
PNC region (Ur≪Ur,crit), concentrations in each size range were approximately constant and
independent ofwind speed and direction. In the wind speed dependent PNC region (Ur≫Ur,crit),
concentrations were inversely proportional to Ur irrespective of any particle size range and
wind directions. The wind speed demarcating the two regimes (Ur,crit) was 1.23±0.55m s−1 for
N10–300, (1.47±0.72 m s−1) for N10–30 but smaller (0.78±0.29m s−1) for N30–300.
Keywords :
Particle number distributionNucleation and accumulationmode particlesTraffic-produced turbulenceStreet canyonParticle dispersionWind-produced turbulence
Journal title :
Science of the Total Environment
Journal title :
Science of the Total Environment