Evaporation 151
4.4 Theory and Mechanisms
4.4.1 Vacuum Evaporation
Reference to the various steps in the formation of a deposit enumerated in the previous section
shows that the theory of vacuum evaporation involves thermodynamic considerations, i.e.
phase transitions from which the equilibrium vapor phase pressure of materials can be derived,
as well as the kinetic aspects of nucleation and growth. Both of these are of obvious
importance in the evolution of the microstructure of the deposit.
The transition of solids or liquids into the gaseous state can be considered to be a macroscopic
or an atomistic phenomenon. The former is based on thermodynamics and results in an
understanding of evaporation rates, source-container reactions and the accompanying effect of
impurity introduction into the vapor state, changes in composition during alloy evaporation,
and stability of compounds. An excellent detailed treatment of the thermodynamic and kinetic
bases of evaporation processes is given by Glang [6]. He points out that the application of
kinetic gas theory to interpret evaporation phenomena resulted in a specialized evaporation
theory. Such well-known scientists as Hertz, Knudsen, and Langnuir were the early workers in
evaporation theory. They observed deviations from ideal behavior which led to refinements in
the theory to include concepts of reaction kinetics, thermodynamics, and solid state theory.
From the kinetic theory of gases, the relationship between the impingement rate of gas
molecules and their partial pressure, p,isgivenby
dN
i
A
e
dt
= (2 πmkT )
−
1
2
p (4.2)
where N
i
is the number of molecules striking a unit area of surface, and A
e
is the area of the
surface.
Hertz [77], in 1882, first measured the evaporation rate of mercury in high vacuum and found
that the evaporation rate was proportional to the difference between the equilibrium vapor
pressure of mercury, p*, at the evaporant surface and the hydrostatic pressure, p, acting on the
surface, resulting from the evaporant atoms or molecules in the gas phase. Thus, the
evaporation rate based on the concept of the equilibrium vapor pressure (i.e. the number of
atoms leaving the evaporant surface is equal to the number returning to the surface) is given by:
dN
i
A
e
dt
(2πmkT )
−
1
2
(p* − p)cm
2
s
−1
(4.3)
such that dN
e
, the number of molecules evaporating from a surface area A
e
in time dt, is equal
to the impingement rate of gas molecules based on the kinetic theory of gases with the value of
p* inserted therein, minus the return flux corresponding to the hydrostatic pressure p of the
evaporant in the gas phase. In the above equations, m is the molecular weight, k is