Rutherford S W
Los Alamos National Laboratory, Engineering Sciences and Applications Division, MS E581, Los Alamos, New Mexico 87545, USA.
Langmuir. 2006 Jan 17;22(2):702-8. doi: 10.1021/la051826n.
Measurements of water adsorption equilibrium in a carbon molecular sieve are undertaken in order to gain insight into the nature of water adsorption in carbon micropores. The measurements are taken at low concentrations to emphasize the role of oxygen-containing functional groups in the adsorption of water. Comparisons are made with previously published water adsorption data at higher concentrations to provide a data set spanning a wide range of loading. The assembled data set provides an opportunity for comparison of various theories for prediction of water adsorption in carbon micropores. Shortcomings of current theories are outlined, and an analytical theory that is free of these deficiencies is proposed in this investigation. With the consideration of micropore volume and pore size distribution, the experimental data and proposed isotherm model are consistent with previous studies of Takeda carbon molecular sieves. Also investigated is the uptake kinetics of water, which is characterized by a Fickian diffusion mechanism. The Maxwell-Stefan formulation is applied to characterize the dependence of the diffusional mobility upon loading.
为了深入了解碳微孔中水分吸附的本质,对碳分子筛中的水吸附平衡进行了测量。测量在低浓度下进行,以强调含氧官能团在水吸附中的作用。将这些测量结果与之前发表的高浓度水吸附数据进行比较,以提供一个涵盖广泛负载范围的数据集。这个组装好的数据集为比较各种预测碳微孔中水吸附的理论提供了机会。概述了当前理论的不足之处,并在本研究中提出了一种没有这些缺陷的分析理论。考虑到微孔体积和孔径分布,实验数据和提出的等温线模型与之前对武田碳分子筛的研究一致。还研究了水的吸附动力学,其特征为菲克扩散机制。应用麦克斯韦-斯蒂芬公式来表征扩散迁移率对负载的依赖性。