The thermal evolution of droplets of aqueous solution of lead nitrate was s
tudied in a drop-tube furnace, which simulates typical conditions for mater
ial synthesis, through spray pyrolysis, and for the thermal destruction of
liquid-containing waste. The processes of droplet evaporation, precursor pr
ecipitation within the droplet and thermolysis of the precipitated particle
s were followed by means of the spectral analysis of the ultraviolet light
scattered by the aerosol produced during the heating of aqueous droplets (1
00 mu m) of lead nitrate, with different salt concentrations, from ambient
temperature up to 1200 K.
Dimensions and physico-chemical properties of the droplets/particles were o
btained in situ by means of ultraviolet spectra of light scattering (UVSLS)
and compared with scanning electron microscopy (SEM) of the sampled materi
al. A plasma generated in the air by an optical breakdown induced by a Nd:Y
AG laser was employed as the light source in the wavelength range 200-400nm
, thus allowing an exceptionally high photon flux in the ultraviolet region
where intense and species-specific interactions with metal species take pl
ace.
The spray drying process was followed by measuring the light transmitted by
the droplets in the backward region. As the drying process progresses, the
surface concentration reaches a saturation value and solute is deposited a
s a solid phase forming a surface crust, which grows steadily. At this poin
t in the process of droplet drying, information was retrieved from the ligh
t reflected by the particle interface. Two spectral scattering behaviors we
re detected at temperatures above the salt precipitation within the droplet
. On the basis of Mie calculations and SEM measurements, these behaviors we
re attributed to lead nitrate particles with typical diameters of the resid
ual droplets (about 50 mu m) and to micrometer-sized lead oxide particles.
The effect of salt concentration on the drying process and the thermolysis
of lead nitrate to oxide was investigated by changing the salt concentratio
n from very dilute conditions up to almost the saturation concentration.