Nanostructure and Salt Effect of Zwitterionic Carboxybetaine Brush at the Air/Water Interface

被引:20
|
作者
Matsuoka, Hideki [1 ]
Yamakawa, Yuta [1 ]
Ghosh, Arjun [1 ]
Saruwatari, Yoshiyuki [2 ]
机构
[1] Kyoto Univ, Dept Polymer Chem, Nishikyo Ku, Kyoto 6158610, Japan
[2] Osaka Organ Chem Ind Ltd, Chuo Ku, Osaka 5410052, Japan
基金
日本学术振兴会;
关键词
STRONG POLYELECTROLYTE BRUSHES; DIBLOCK COPOLYMER MONOLAYERS; AQUEOUS-SOLUTION PROPERTIES; STATIONARY-PHASE; SURFACE-ACTIVITY; WATER; POLY(SULPHOPROPYLBETAINES); TRANSITION; MICELLES; POLYMERS;
D O I
10.1021/acs.langmuir.5b00637
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Zwitterionic amphiphilic diblock copolymer, poly(ethylhexyl acrylate)-b-poly(carboxybetaine) (PEHA-b-PGLBT), was synthesized by the reversible addition-fragmentation chain transfer (RAFT) method with precise control of block length and polydispersity. The polymers thus obtained were spread onto the water surface to form a polymer monolayer. The fundamental property and nanostructure of the block copolymer monolayer were systematically studied by the surface pressure-molecular area (pi-A) isotherm, Brewster angle microscopy (BAM), and X-ray reflectivity (XR) techniques. The pi values of the monolayer increased by compression in relatively larger A regions. After showing a large plateau region by compression, the pi value sharply increased at very small A regions, suggesting the formation of poly(GLBT) brush formation just beneath the water surface. The domain structure of mu m size was observed by BAM in the plateau region. XR profiles for the monolayer at higher surface pressure regions clearly showed the PGLBT brush formation in addition to PGLBT carpet layer formation under the hydrophobic PEHA layer on the water surface, as was observed for both anionic and cationic brush layer in the water surface monolayer studied previously. The critical brush density, where the PGLBT brush is formed, was estimated to be about 0.30 chains/nm(2) for the (EHA)(45)-b-(GLBT)(60) monolayer, which is relatively large compared to other ionic brushes. This observation is consistent with the fact that the origin of brush formation is mainly steric hindrance between brush chains. The brush thickness increased by compression and also by salt addition, unlike the normal ionic brush (anionic and cationic), whose thickness tended to decrease, i.e., shrink, by salt addition. This might be a character unique to the zwitterionic brush, and its origin is thought to be transition to an ionic nature from the almost nonionic inner salt caused by salt addition since both the cation and anion of the GLBT chain obtained counterions by the addition of salt. This stretching nature of the PGLBT brush depends on the ion species of the salt added, and it followed the Hofmeister series, i.e., more stretching in the order of Li+ > Na+ > K+. However, it was rather insensitive to the anion species (Cl-, Br-, SCN-), which suggests that the carboxylic anion has a more dominant effect than the quaternized cation in GLBT although the former is a weak acid and the latter is believed to be a strong base.
引用
收藏
页码:4827 / 4836
页数:10
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