Nuclear magnetic resonance imaging (NMRI) techniques were used for the
measurement of the spatial distribution of apertures and two-phase fl
uid distributions in rock fractures. Rock models of known apertures we
re used to validate the NMRI technique. NMRI aperture values were in g
ood agreement with nominal and hydraulic aperture values. The fracture
signal in porous rock was isolated by NMR spin-spin relaxation times.
Areal distributions of oil and water in an immiscible fracture flow w
ere resolved on the basis of their NMR spin-lattice relaxation times.