Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
596360 | Colloids and Surfaces A: Physicochemical and Engineering Aspects | 2008 | 5 Pages |
Surface pressure versus specific molecular area (π–A) isotherms of stearic acid monolayers have been studied by varying the pH of the aqueous subphase containing monovalent (Na) or different divalent (Mg, Ca, Ba, Zn and Cd) cations. The lowering of the tilted to untilted phase transition pressure (πt) with increasing pH of the subphase is correlated with an increase of the headgroup dissociation of the acid monolayer. On pure water, the surface pressure drops after the collapse point (πc) to a lower pressure value (πl). The pressure-gap Δπ = πc − πl changes with increasing dissociation, depending upon the particular cation. After a certain pH, no pressure gap is observed and π remains constant or increases slowly after πc. This transition from constant area collapse to constant pressure collapse of the monolayer is observed for all monovalent and divalent cations near total monolayer dissociation.