Chemistry · Ch 10 — Surface Chemistry
Freundlich Adsorption Isotherm
Freundlich Adsorption Isotherm
Adsorption isotherms can also be examined quantitatively: a plot of the amount of adsorbate adsorbed against the pressure (or, for adsorption from solution, the concentration of the adsorbate) at constant temperature is called an adsorption isotherm, and several mathematical equations have historically been proposed to fit its shape — the Freundlich isotherm being the earliest and most widely used.
According to Freundlich, the amount x of adsorbate adsorbed per gram m of adsorbent, at a pressure p and constant temperature, follows the empirical relationship
where k and n are empirical constants (introduced by Freundlich) that depend on the particular adsorbent–adsorbate pair and on temperature, and n is always found to be greater than unity, so the exponent is always a positive fraction less than one. This equation applies directly to the adsorption of gases on solid surfaces; when instead applied to adsorption from solution, pressure p is simply replaced by the concentration c of the adsorbate in solution, giving the equivalent form . Either version quantitatively predicts how the amount adsorbed responds to changing pressure (or concentration) at fixed temperature — and in particular predicts that x/m keeps increasing as pressure rises, though with steadily DIMINISHING returns, since raising p to a fractional power less than one produces ever-smaller proportional gains as p grows.
Because the equation as written is not linear, it is normally tested and used in its logarithmic form, obtained by taking logarithms of both sides:
Plotting on the vertical axis against on the horizontal axis therefore gives a straight line, whose SLOPE equals and whose Y-INTERCEPT equals — precisely the two constants of the original Freundlich equation, now readable directly off a straight-line graph constructed from a handful of experimental (p, x/m) readings. …
What this figure shows. Two related plots illustrate the Freundlich equation. The direct plot of x/m against p is a curve that rises steeply at first and then flattens out — a shape the equation reproduces, since raising a small p to a fractional power (with n always greater than unity, so ) gives diminishing returns as p grows, matching the observed saturation-like flattening at higher pressure. Taking logarithms of both sides converts this curve into a straight line: . Plotting on the vertical axis against on the horizontal axis gives a straight line whose slope equals and whose y-intercept equals — this linear form is exactly what makes k and n expe …