This paper reports an experimental study conducted on turbulent jet propane
flames aiming at further understanding of turbulent structure in non-premi
xed slow-chemistry combustion systems. Measurements of mean and fluctuating
velocity and temperature fields, mean concentration of major chemical spec
ies, correlation between velocity and temperature fluctuations, and dissipa
tion of temperature fluctuations are reported in a turbulent round jet non-
premixed propane flame, Re = 20 400 and 37 600, issuing vertically in still
air. The experimental conditions were designed to provide a complete defin
ition of the upstream boundary conditions in the measurement domain for the
purpose of validating computational models. The measured data depicts usef
ul flow field information for describing turbulent non-premixed slow-chemis
try flames. Velocity-temperature correlation measurements show turbulent he
at fluxes tended to be restricted to the mixing layer where large temperatu
re gradients occurred. Observations of nongradient diffusion of heat at x/D
= 10 were verified. Temperature fluctuation dissipation, ii, showed the hi
ghest values in the shear layer, where the variance of temperature fluctuat
ions was maximum and combustion occurred. The isotropy between the temperat
ure dissipation in the radial and tangential directions was confirmed. By c
ontrast, the observed anisotropy between axial and radial directions of dis
sipation suggests the influence of large structures in the entrainment shea
r layer on the production of temperature fluctuations in the flame region.
The value of the normalized scalar dissipation at the stoichiometric mixtur
e fraction surface, chi (st), was calculated, and ranges between 2 and 4 s(
-1). The measured data were used to estimate the budgets in the balance equ
ations for turbulent kinetic energy, Reynolds shear stresses, turbulent hea
t flux and temperature variance, quantifying the mechanisms involved in the
generation of turbulence as well as in the transport of the temperature. (
C) 2000 Elsevier Science Inc. All rights reserved.