We introduce a rapid, quantitative nuclear magnetic resonance imaging
(NMRI) technique to resolve and measure multiple fluid phases in porou
s media. Liquids are resolved on the basis of their NMR spin-spin (T-2
) relaxation times, and their intensities are corrected by attenuation
analysis. The phase-resolved and corrected NMRI intensities are norma
lized to yield fluid saturations. We present the procedure and limitat
ions of this technique. We present in-situ saturation measurements for
three immiscible (oil and water) displacements in the same Berea sand
stone core. We compared NMRI: and effluent recovery methods. T-2 of th
e displacement fluids were sensitive to displacement conditions.