Rj. Brown et Rw. Bilger, EXPERIMENTS ON A REACTING PLUME - 1 - CONVENTIONAL CONCENTRATION STATISTICS, Atmospheric environment, 32(4), 1998, pp. 611-628
Experiments have been carried out under laboratory conditions to study
turbulent mixing with chemical reaction. Such flows are common in the
environment but there are few high-resolution measurements of them un
der controlled conditions. The reaction NO + O-3 --> NO2 + O-2 + 200 k
J (mel)(-1) (in the absence of UV radiation) has been used by introduc
ing a non-buoyant reactive plume of NO into a turbulent grid flow dope
d with O-3. The experiments have been conducted over a wide range of c
onditions by varying the Damkohler number (the ratio of the flow times
cale to that of the chemical reaction) by a factor of 6 and varying th
e ratio of initial reactant concentrations by a factor of 30. The data
are presented in two parts. Part 1 (present paper) presents conventio
nal concentration statistics. Part 2 presents concentration statistics
conditionally averaged by a mixing parameter and discusses their usef
ulness for investigating the reactive behaviour of the plume. Speciall
y developed chemiluminescent analysers are used to measure NO and O-3
concentrations with high-frequency response and a spatial resolution o
f four Kolmogorov scales (in this flow). The mixing field of the plume
is studied using conserved scalar theory and is compared to that obta
ined in other non-reactive flows. Results for the means, variances and
joint statistics of the reactive species are presented and compared w
ith frozen and equilibrium limits obtained from the conserved scalar t
heory for reacting flows. Statistics for NO show no significant trend
with Damkohler number while those for O-3 and NO2 have increased react
ion at higher Damkohler number. The reactive scalar means are bounded
by the frozen and equilibrium limits as they should be according to co
nserved scalar theory. Other reactive scalar statistics are not necess
arily bounded by the limits. A simple relation between moments of O-3
and NO2 is found in the experimental results and is confirmed by conse
rved scalar theory. Contribution to the mean reaction rate from the re
actant covariance and product of means is compared and it is found tha
t both are significant under the present conditions. Intensity of segr
egation varies over a wide range and is sensitive to initial reactant
concentrations. (C) 1998 Elsevier Science Ltd. All rights reserved.