The present research focuses on studying an isothermal spray to understand the
mechanism of interaction between droplets and turbulent air flow, and an evaporative
spray to evaluate the group evaporation of droplets as opposed to single droplet
evaporation. The thesis describes the development and application of two novel
experimental techniques for simultaneous characterization of droplet and gaseous
phases in isothermal and evaporative sprays respectively. Both approaches use the
out-of-focus imaging technique, Interferometric Laser Imaging for Droplet Sizing
(ILIDS), for planar measurements of droplet size and velocity. The in-focus imaging
techniques Particle Image Velocimetry (PIV) and Planar Laser Induced Fluorescence
(PLIF) are respectively combined with ILIDS for simultaneous measurement of gas
flow characteristics in an isothermal spray and vapour concentration distribution in
an evaporative spray.
Combination of either of the two optical arrangements results in a discrepancy in the
location of the centre of a droplet leading to erroneous identification of the droplets
in the PIV/PLIF images. This issue has been addressed and a method is proposed
to reduce the droplet positioning error.
The coupling between the droplet and gas phases in the isothermal spray is explained
by evaluating several statistical quantities, the most important being the spatial
correlation coefficients of the droplet-gas velocity fluctuations obtained conditional on
droplet size classes. The effect of anisotropy and gravity on the momentum transfer
between the two phases are studied. The gas flow eddy structures are extracted by
applying Proper Orthogonal Decomposition (POD) on the instantaneous gas velocity
data and the selective influence of the large scale eddy structures of the gas phase
flow on the droplet-gas flow interaction are examined.
In order to study the effect of inter droplet spacing on the droplet evaporation rate,
experiments are first performed for the mono-sized droplet stream. The smaller inter
droplet spacing of the larger droplet sizes causes the vapour to surround the droplet
stream leading to droplet group evaporation. The smaller magnitude of the mean
group evaporation number, evaluated at different radial locations in the evaporative
acetone spray, suggests the mode of evaporation is in the range of regimes of individual
to group evaporation. It is shown that the assumption of uniform droplet spacing in
the theoretical expressions for the evaluation of the group evaporation number always
leads to overestimation of the group evaporation number.