Morphology of porous media studied by nuclear magnetic resonance line shapes and spin-echo decays

Citation
Sg. Allen et al., Morphology of porous media studied by nuclear magnetic resonance line shapes and spin-echo decays, J CHEM PHYS, 114(7), 2001, pp. 3258-3264
Citations number
29
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF CHEMICAL PHYSICS
ISSN journal
00219606 → ACNP
Volume
114
Issue
7
Year of publication
2001
Pages
3258 - 3264
Database
ISI
SICI code
0021-9606(20010215)114:7<3258:MOPMSB>2.0.ZU;2-6
Abstract
The line shape and spin-echo decays of liquids confined in small pores have been studied as a function of saturation. The samples used were of silica with nominal pore diameters of 60, 200, and 500 Angstrom and had been satur ated either with cyclohexane or water. The proton nuclear magnetic resonanc e linewidth and peak shift were measured as a function of saturation. For w ater samples the peak shift increased and linewidth decreased up to a criti cal saturation level above which the peak shift decreased and linewidth inc reased. This critical saturation point occurs when the surface layer is com plete, and is related to the morphology of the pores. It provides evidence to suggest that the internal surface of the 200 Angstrom silica sample was more irregular than the 60 Angstrom sample. For the cyclohexane samples the peak shift increased and the linewidth decreased with saturation. The spin -echo amplitude decays were found to be faster than those seen in previous work. This is attributed to diffusion through a range of field gradients ca used by susceptibility variations within the system. The nature of such var iations depends on the saturation level. The decays were fitted to a stretc hed exponential function. Values for the average field gradients and the st retching parameter provide a measure of the range of gradients found and ha ve been deduced for each experiment. Most information on the internal pore morphology is found by studying the systems at low levels of water content. The average field gradient and the stretching exponent may be related to t he pore morphology. (C) 2001 American Institute of Physics.