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MORPHOLOGY OF POROUS MEDIA STUDIED BY NUCLEAR MAGNETIC RESONANCE

机译:核磁共振研究多孔介质的形态

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The filling processes of water and cyclohexane in porous silica (40 Angstrom, 60 Angstrom and 112 Angstrom pore size samples) were studied using T-2 nuclear magnetic resonance (n.m.r.) experiments. The silica pores contained water or cyclohexane and the experiments were performed at room temperature and at filling fractions ranging from 0.02 to 1.0 (that is, completely full). Two distinct processes were observed which depended on the hydrophilicity of the silica surface (or the surface adhesion of the liquid). Water was found to collect in small puddles in the silica interstices, and to form a surface layer over the silica before the remaining pore volume was filled, Water in a surface-treated porous silica and cyclohexane in regular porous silica appeared to completely fill the smaller be-Fore the larger pores, and not form a separate surface-coating layer. This work also presents the techniques used to calculate quantitative information about the filling process; specifically, determination of the volume to surface-area ratio of the liquid puddles as well as the number of these puddles, is demonstrated. (C) 1997 American Institute of Physics. [References: 16]
机译:使用T-2核磁共振(n.m.r.)实验研究了多孔二氧化硅(40埃,60埃和112埃孔径样品)中水和环己烷的填充过程。二氧化硅孔中含有水或环己烷,实验是在室温下进行的,填充分数为0.02至1.0(即完全充满)。观察到两个不同的过程,这取决于二氧化硅表面的亲水性(或液体的表面粘附力)。发现水聚集在二氧化硅间隙中的小水坑中,并在填充剩余的孔体积之前在二氧化硅上形成了一个表面层。表面处理的多孔二氧化硅中的水和常规多孔二氧化硅中的环己烷似乎完全填满了较小的水。在较大的孔之前出现,并且不形成单独的表面涂层。这项工作还介绍了用于计算有关填充过程的定量信息的技术。具体地,说明了确定液体水坑的体积与表面积之比以及这些水坑的数量。 (C)1997美国物理研究所。 [参考:16]

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