rate going on = k1 C ( 1 - F )
The evaporation from the surface is proportional to the amount of surface covered:
rate leaving = k2 F
where k1 and k2 are rate coefficients
C = concentration in the fluid
F = fraction of the surface
covered
Animation of finding adsorption sites
At equilibrium, the two rates are equal, and we find that:
By dividing the numerator and denominator by k1, and making use of the fact that q will be proportional to F, the useful form of the equation is:
where qm = q for a complete
monolayer
Ka = a coefficient
Taking reciprocals and rearranging: ( details of math for sleepy people)
A plot of
versus
should indicate a straight line of slope
and an intercept of
. The
graph shows data points and lines fitted to both Freundlich and Langmuir
equations.