Guillermo Armel, Gebel Gérard, Mendil-Jakani Hakima, Pinton Eric
CEA, INAC, SPrAM (UMR5819 CEA/CNRS/UJF), 38054 Grenoble Cedex9, France.
J Phys Chem B. 2009 May 14;113(19):6710-7. doi: 10.1021/jp8110452.
The water uptake and the water self-diffusion coefficient were measured in Nafion membranes at subzero temperatures. NMR spectroscopy was used to precisely quantify the actual concentration of water in membranes as a function of the temperature and their hydration rates at room temperature. We find that below 273 K the water concentration decreases with temperature to reach, at around 220 K, a limit value independent of the initial concentration. This regime is observed if the concentration at room temperature is higher than 10%. Below this concentration no membrane deswelling was observed. The water self-diffusion coefficient, measured by pulsed field gradient NMR in function of the temperature, is determined by the actual concentration C(T) whatever the concentration at room temperature. The concentration variation is attributed to a decrease in the relative humidity RH(T) of the water vapor surrounding the membrane induced by the simultaneous presence of supercooled water inside the membrane and ice outside the membrane.
在零下温度下测量了Nafion膜的吸水率和水的自扩散系数。利用核磁共振光谱精确量化了膜中实际水浓度随温度的变化以及它们在室温下的水合速率。我们发现,在273K以下,水浓度随温度降低,在约220K时达到一个与初始浓度无关的极限值。如果室温下的浓度高于10%,则会观察到这种情况。低于此浓度时,未观察到膜的溶胀。通过脉冲场梯度核磁共振测量的水自扩散系数随温度的变化,无论室温下的浓度如何,都由实际浓度C(T)决定。浓度变化归因于膜内过冷水和膜外冰的同时存在导致膜周围水蒸气相对湿度RH(T)的降低。