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The new NMR method, demonstrated in the present work, allows within local small volumes the determination of integral structural parameters like the surface-to-pore volume ratio or the tortuosity of a fluid-filled porous medium. A combination of conventional imaging (MRI) with measurements of observationtime dependent self-diffusion (dynamic imaging) was used.

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Systematic experimental studies focusing on the practical application of observation time dependent pulsed-field-gradient (PFG) NMR were performed. The objective was to provide engineering scientists with a reliable experimental tool for characterizing the structure and transport in fluid-filled porous media. Observation time dependent self-diffusion in glass bead packs as model systems was investigated, where the diffusing species (molecules of the solvent or dissolved particles) served as probes for the confining geometry in the porous medium. First, the basic question whether the obtainable structure information is independent of the actual mobility of the diffusing probe particles was examined experimentally. It could be demonstrated that plotting the normalized time-dependent diffusion coefficient D(t)/D 0 versus the actual migration length l D (t) during a given observation time t indeed yields a characteristic "master curve" that is independent of the mobility of the diffusing species, thus reflecting, as desired for a reliable method, solely the effects of the confining geometry of the porous system of interest. It was further shown that from the master curve a new quantity, i.e., a "characteristic inner length" or "correlation length" n D can be derived that corresponds to a path length in the porous medium, after which particles in the pore fluid experience an averaged restricting geometry and diffuse with an effective diffusion coefficient D eff . It turned out that n D is surprisingly short, that is, in the order of the bead radius. Moreover, it was demonstrated that normalization of this migration length with the bead radius yields a common master curve for all monodisperse bead packs used and thus, it is obviously possible to derive and record master curves for different kinds of packs, beds or other porous media as references that can be used to characterize or certify the kind of the porous matrix of interest.