© A.W.Marczewski 2002

A Practical Guide to Isotherms of ADSORPTION on Heterogeneous Surfaces

General Integral Equation of Adsorption:

Dilute single-solute adsorption

see G.I.E.A. for single gas and binary liquid adsorption

see G.I.E.A. for multicomponent adsorption

isotherm equations |
GL isotherm

GL energy distribution |
energy dispersion |
Global Heterogeneity

General Integral Equation | Monolayer ( Local isotherm | Lateral Interactions ) | Multilayer

**NOTE**

*Equations below are good e.g. for dilute solutions of organics. If you deal with weakly soluble solutes (or your concentrations are close to solubility limit, c _{s}) you should take it into account, e.g. by using "multilayer correction" - see below. Dilute single-solute adsorption is a special case of binary liquid mixture adsorption where one of the components (solvent) is present in the solution bulk in almost constant concentration.*

**General Integral Equation of Adsorption** (GIE) is a general formulation of adsorption isotherm involving energetical heterogeneity of the adsorption system (i.e. adsorbate-surface). (One has to be always aware that in the case of solutions the observed adsorption effect is always an exchange of molecules - adsorbate solute for solvent molecule and *vice versa* - competitive adsorption).

The first attempt to describe adsorption on non-homogeneous solids was by Langmuir (1918) but it was represented by a simple summation not an integral. Another similar in character **Integral Equation of Adsorption** is the Stoeckli integral equation for adsorption on microporous non-uniform solids.

**General Integral Equation of Adsorption**

For dilute single-solute adsorption

(see GIE for gas and binary liquid adsorption or multicomponent adsorption)

where: θ_{t} is global (overall) adsorption isotherm (overall coverage) and θ_{l} is local adsorption isotherm (local coverage), χ(E) is energy distribution function (see χ(E) functions and χ(E) model pictures for GL isotherm) and E is reduced adsorption energy (E=ε/RT where ε - energy). For many theoretical isotherms energy range extends from -∞ to +∞. It is not physically consistent, but with some notable exceptions (e.g. Sq isotherm), global isotherms obtained for limited energy range have no simple analytical representations.

**Energy distribution function**

see also:

a section in General Integral Equation of Adsorption (simple cases)

General Integral Equation of Adsorption (multicomponent)

Energy correlation (competition: solute vs. solvent)

Adsorption basics (gas vs. liquid vs. solute adsorption)

CAUTION!

One has to be always cautious while describing energy distribution function as the property of adsorbent only. Though for homogeneous adsorbents it may be true, it may change not only with the change of such adsorbate properties like functional groups, but also with changing molecular size, shape and surface topography. Moreover, in adsorption of mixtures the obtained energy distribution function may have altered - and quite different - shape and width depending on energy correlations for molecule pairs on adsorption sites.

**Monolayer**

**Local Langmuir isotherm:**

*Localised monolayer physical adsorption (another local isotherm may be e.g. Jovanovic eq.):*

where: K_{o} is entropy-related and temperature dependent constant (so-called pre-exponential factor), sites are characterised by reduced energy E (or rather reduced energy of adsorption of a given molecule on certain site is E).

**Local Langmuir isotherm with lateral interactions** included:

where: f_{int}(θ_{x}) denotes interaction factor and θ_{x} is relative surface coverage (local or overall depending on surface topography):

for **random site topography**: θ_{x}=θ_{t} (global coverage)

for **pathwise topography**: θ_{x}=θ_{l} (local coverage).

Surface site **topography** and lateral interactions:

The reason for such a difference is that on random topography surfaces the interaction factor depends on the mean field of adsorbate molecules which is surface-averaged anyway, i.e. it depends on the local average adsorbate density which is the same as average density of adsorbate molecules over the whole surface (that is: θ_{l,avg} = θ_{t}) and thus does not depend on which particular site the molecule is sitting (i.e. does not depend on local adsorption energy E).
However, for patchwise topography, the density of adsorbate molecules is characteristic - and different (depending on the local adsorbate density, i.e. local coverage θ_{l}) - for each of the patches characterized with different adsorption energy E.

For *(simplified)* **Kiselev** (association, i.e. specific lateral interactions in surface phase) and **Fowler-Guggenheim** (Van der Waals, i.e. non-specific lateral interactions in mean field approximation) we get interaction factors, respectively:

(Kiselev)

(Fowler-Guggenheim)

The above Kiselev interaction form is a simplified equation, the form of **full Kiselev** equation is more complicated and may involve also lateral non-specific (FG mean-field) interactions:

This factor may be simplified in some cases:

for K_{n}θ_{x} >> 1 :

for K_{n}θ_{x} << 1 :

One may also see, that the association constant K_{n} in simplified Kiselev equation has an approximate value of 2K_{n} of the full Kiselev equation (if of course we assume that non-specific interaction term α=0).

**NOTE on random/patchwise topographies.**

If for a given type of heterogeneity and without lateral interactions present the isotherm equation θ_{t}(c) has analytical form, it will be analytical with lateral interactions and **random site topography**, too. New isotherm θ_{t,int}(c) will have indentical form as the original equation if we replace concentration (or pressure for gas adsorption) by a suitable term c' = c f(θ_{t}).
For **patchwise topography** with lateral interactions the obtained isotherms are generally non-analytical.

**Multilayer**

**Local Langmuir + multilayer isotherm**, where x=c/c_{s} :

For BET model (See other multilayer isotherms) a **multilayer factor** f_{multi}(x) is:

**Global/overall multilayer isotherm** is easily obtained from its monolayer form θ_{t}(c) by replacing c with c/(1-x) and including f_{multi}(x):

isotherm equations | GL isotherm

GL energy distribution | energy dispersion | Global Heterogeneity

Top

My papers

Search for papers

Main page

Send a message to *Adam.Marczewski AT@AT umcs.lublin.pl*