A common occurence in the atmosphere is the deposition of water
vapor
on salt particles at moderate relative humidities, forming a film
of water around the salt core. It can be shown that as the humidity
rises, there will be a deliquescent point (dependent on the salt but
around 70 to 80% RH) where the salt will disolve creating a haze
particle.
Consider the evolution of such a droplet at fixed
and
. Let
the droplet have density
, radius
and surface tension
. Let the concentration of salt molecules in
solution
(assume the solution is ideal) be
where
and
are the numer of salt and water molecules,
respectively.
Let
be the mass of the salt nucleus and
and
be the molecular weights of salt and water.
Assume
where
- Show that in a dilute solution
,
where
depends
on
,
,
, the salt mass and
and
,
and write
in terms of
,
and these variables assuming the solution is dilute.
- Find
, the free energy in a system containing
vapor molecules
and
molecules of water in a salt solution drop of
radius
,
and activity
.
- Find the relationship between
, the
equilibrium droplet radius
and the supersaturation
.
- Find the equilibrium vapor pressure over the drop,
in terms of
and the other parameters
of the problem.
- Sketch the curves (the Kohler curves)
vs.
for constant
and several values
of
.
- Find the values of
and
at
the maximum point of the curve, (where
). Is the equilibrium at this
point stable or unstable?
Why?