Separation of fine coal in froth flotation relies upon the
wettability difference between the
coal-rich and mineral-rich particles in the aqueous solution. Two
methods were used to measure
the wettability of six ranks of coal as well as coal samples treated
with various levels of dispersed
collector in aqueous solution. Wettability was determined by
measuring the distribution of critical
wetting surface tension, i.e., surface energy, using the film flotation
technique and by measuring
the induction time, i.e., bubble−particle attachment time, of the
material. The wetting of coal
particles is strongly dependent upon the coalification processes and
can be affected by ash content.
For anthracite coal with a high ash content, very high surface
energy and intermediate induction
time were measured, but intermediate floatability with a very good ash
rejection was obtained.
Sub-bituminous coal with low mineral inclusion was found to have a
relatively low surface energy,
and thus a high floatability, but very poor selectivity was observed,
which was reflected in
lengthened induction time. When dynamics of flotation behaviors
are involved, flotation results
can be better interpreted by induction time. For dispersed
collector-treated coal samples, an
increase in collector dispersion (i.e., a decrease in kerosene droplet
size), by direct liquid collector
mechanical agitation, ultrasonic energy emulsification, or atomization,
caused decreases in surface
energy and induction time and closely matched the increase of flotation
recovery and selectivity.
With similar particle density, mineral liberation conditions, and
particle size, the induction time
was found to be closely related to the mean critical surface tension
for untreated coal samples
and for HV-bituminous coal samples treated by various levels of
dispersed collector.