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Effect of the exchange of substituent position in an amide amphiphile on the monolayer characteristics
Authors:Vollhardt D  Wagner R
Institution:Max Planck Institute of Colloids and Interfaces, D-14424 Potsdam/Golm, Germany, and GE Bayer Silicones Technology, 51368 Leverkusen, Germany. vollh@mpikg-golm.mpg.de
Abstract:The monolayer characteristics of two very similar amphiphiles, N-tridecyl-beta-hydroxypropionic acid amide (C13H27-NH-CO-C2H4OH; THPA) and N-(beta-hydroxyethyl)tridecanoic acid amide (C13H27-CO-NH-C2H4OH; HETA), the chemical structure of which is only changed by exchanging the position of the two substituents at the acid amide group, are compared. These small changes in the chemical structure give rise to large differences in the phase behavior of the HETA and THPA monolayers, as concluded from the differences in the surface pressure-area (pi-A) isotherms. Since both amphiphiles have the same alkyl chain length, the shift of the fluid/condensed phase transition pressure pi(c) to higher temperatures from THPA to HETA indicates a stronger polar character of the THPA headgroup. Considerable differences between the HETA and THPA monolayers also exist in the domain morphology, although, in both cases, six arms usually grow from a round center. The fractal-shaped HETA domains grow by tip splitting under the formation of numerous doubloons so that branching is considerably limited. This suggests a certain fluidity of the HETA condensed phase. The main differences of the domains result from the higher crystallinity. The starlike THPA domains have dendritic character and can form curved dendrites, which are partially two-dimensional twins due to the formation of dislocations in the two-dimensional lattice structure. In the case of HETA monolayers, the grazing incidence X-ray diffraction studies reveal a hexagonal packing of the alkyl chains oriented perpendicularly to the surface in an LS phase. In the case of THPA monolayers, an oblique lattice is formed. However, at low temperatures, a second phase transition between two condensed phases occurs that is demonstrated by an abrupt transition between two different oblique lattice structures at the surface pressure where a cusp in the pi-A isotherms occurs at T < 10 degrees C.
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