Single-Molecule Studies of Diffusion by Oligomer-Bound Dyes in Organically Modified Sol−Gel-Derived Silicate Films

尼罗河红 化学 硅酸盐 荧光相关光谱 扩散 分子 荧光 红豆 分析化学(期刊) 尼罗河蓝 荧光光谱法 束缚水 有机化学 纳米技术 溶胶凝胶 材料科学 热力学 物理 量子力学
作者
Skylar Martin‐Brown,Yi Fu,Ginagunta Saroja,Maryanne M. Collinson,Daniel A. Higgins
出处
期刊:Analytical Chemistry [American Chemical Society]
卷期号:77 (2): 486-494 被引量:44
标识
DOI:10.1021/ac0491511
摘要

Single-molecule fluorescence spectroscopy is used to study dye diffusion within organically modified silicate (ORMOSIL) films. ORMOSIL films are prepared from sols containing tetraethoxysilane and isobutyltrimethoxysilane in 2:1 and 1:9 molar ratios. Nile red and a new silanized form of nile red that can be covalently attached to the silicate matrix are used as fluorescent probe molecules. The number and rate of single molecules diffusing through these films increases dramatically with increasing film organic content. Autocorrelation of the fluorescence images yields a quantitative measure of the relative populations of fixed and diffusing species. Surprisingly, both "free" and silicate-bound nile red exhibit relatively facile translational motions. Single-molecule/single-point fluorescence correlation spectroscopy (FCS) is used to measure the dye diffusion coefficients in submicrometer-scale film regions. The most common diffusion coefficients for "free" and silicate-bound nile red molecules in the 1:9 films are 3.9 x 10(-10) and 1.6 x 10(-10) cm(2)/s, respectively. The unexpectedly rapid diffusion of silicate-bound nile red is attributed to the presence of liquidlike silicate oligomers in the films. A lower bound for the molecular weight of the oligomers is estimated at 2900. Bulk solution-phase FCS experiments performed on "free" and silicate-bound nile red species extracted into chloroform solutions provide valuable support for these conclusions. Comparison of the results derived from experimental and simulated time transients indicates film heterogeneity occurs on sub-100-nm-length scales and likely results from the presence of inorganic- and organic-rich domains.

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