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ATR-FTIR observations of water structure in colloidal silica: Implications for the hydration force mechanism

机译:胶体二氧化硅中水结构的ATR-FTIR观察:对水合力机理的启示

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Attenuated total internal reflection Fourier-transform infrared spectroscopy (ATR-FTIR) was used to probe the change in water structure in silica colloids as a function of particle density. The absorption index (k) spectra were calculated from the ATR spectra using the subtractive Kramers-Kronig transform in order to avoid the effects of the density-dependent refractive index on the raw spectra and allow direct comparison of the different chemical environments. Normalized difference spectra were obtained by subtracting the k spectrum of bulk water from those of the silica colloids. At low particle densities, these difference spectra reveal the presence of a strongly hydrogenbonded hydration layer at the surface of the colloidal particles. At higher particle densities, the hydrogen-bonding network is increasingly disrupted. The results provide direct experimental evidence of hydrogen-bond breaking as the mechanism for the hydration force, which provides the extraordinary stability of colloidal silica.
机译:衰减全内反射傅里叶变换红外光谱(ATR-FTIR)用于探测二氧化硅胶体中水结构随颗粒密度变化的变化。使用减法Kramers-Kronig变换从ATR光谱计算吸收指数(k)光谱,以避免密度依赖性折射率对原始光谱的影响,并允许直接比较不同的化学环境。通过从二氧化硅胶体的k光谱中减去散装水的k光谱获得归一化的差异光谱。在低颗粒密度下,这些差异光谱揭示了在胶体颗粒表面存在强氢键合水合层。在较高的颗粒密度下,氢键网络越来越受到破坏。结果提供了氢键断裂作为水合力机理的直接实验证据,这提供了胶体二氧化硅非凡的稳定性。

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