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Investigating hydration dependence of dynamics of confined water: Monolayer, hydration water and Maxwell-Wagner processes

机译:研究承压水动力学的水合依赖性:单层水合水和麦克斯韦-瓦格纳过程

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The dynamics of water confined in silica matrices MCM-41 C10 and C18, with pore diameter of 21 and 36 angstrom, respectively, is examined by broadband dielectric spectroscopy (10(-2)-10(9) Hz) and differential scanning calorimetry for a wide temperature interval (110-340 K). The dynamics from capillary condensed hydration water and surface monolayer of water are separated in the analysis. Contrary to previous reports, the rotational dynamics are shown to be virtually independent on the hydration level and pore size. Moreover, a third process, also reported for other systems, and exhibiting a saddlelike temperature dependence is investigated. We argue that this process is due to a Maxwell-Wagner process and not to strongly bound surface water as previously suggested in the literature. The dynamics of this process is strongly dependent on the amount of hydration water in the pores. The anomalous temperature dependence can then easily be explained by a loss of hydration water at high temperatures in contradiction to previous explanations. (c) 2008 American Institute of Physics.
机译:通过宽带介电谱(10(-2)-10(9)Hz)和差示扫描量热法检测分别限制在孔径分别为21和36埃的二氧化硅基质MCM-41 C10和C18中的水的动力学。较宽的温度间隔(110-340 K)。分析中分离了毛细管冷凝水化水和表面单层水的动力学。与以前的报告相反,旋转动力学显示出实际上与水合程度和孔径无关。此外,还研究了第三种方法,该方法也针对其他系统进行了报道,并且显示出类似鞍形的温度依赖性。我们认为该过程是由于麦克斯韦-瓦格纳过程所致,而不是象文献先前所建议的那样强烈地结合了地表水。该过程的动力学很大程度上取决于孔中的水合水量。与以前的解释相反,在高温下失去水合水很容易解释异常的温度依赖性。 (c)2008年美国物理研究所。

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