Pulsed laser Mie scattering and laser Doppler velocimetry (LDV), both conditioned on the origin of the seed particles, have been successively performed in turbulent jets with variable density. In the early stages of the jet developments, significant differences are measured between the ensemble average LDV data obtained by jet seeding and those obtained by seeding the ambient air. Careful analysis of the marker statistics shows that this difference is a quantitative measure of the turbulent mixing. The good agreement with gradient-diffusion modelling suggests the validity of a general diffusion equation where the velocities involved are expressed in terms of ensemble conditional Favre averages. This operator accounts for all events (including intermittent ones) and for variations in the density of the marked fluid whose velocity is still specified by the binary origin of the marker.
List of symbolsFroude number J diffusion vector, m/s k global sensitivity of the detection system for one particle (signal level) N P number of seed particles in the probe volume N P,i number of seed particles in sample i N P N id number of ideal particles N id * number of marked ideal particles P* probability that an ideal particle be marked by a seed particle P(qz) probability density function for qz, m 3 /kg P ðN P ¼kÞ probability to have k seed particles in the probe volume P ðN P ¼k qzÞ j probability of having k seed particle conditioned on a given value of qz r radial coordinate, m R q =q (1) /q (2) , density ratio S 1 local signal level with jet seeding S 1