Determining pore sizes using an internal magnetic field
A concept is proposed to measure the pore size length scale by the internal magnetic field (B(i)) in porous materials. The spatial distribution of the magnetic field inhomogeneity, a result of the magnetic susceptibility contrast between the porous material and the fluid, reflects the underlying pore geometry. Diffusion in B(i) causes the initial decay of magnetization. At long times, the effect of B(i) saturates when the diffusion length reaches a characteristic pore size. This method is independent of surface spin relaxation in determining pore sizes. Nuclear magnetic resonance experiments on packed glass beads and sedimentary rock samples will be presented. Copyright 2000 Academic Press.
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