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High power proton relaxometry was applied to investigate the liquid phase contained in porous rock. Proton free induction decays and spin-lattice relaxation times allowed us to investigate the pore distribution and the contribution of mobile and of immobilized liquid. The differences in pore distributions in oil-containing limestone and in Weglowicki sandstone were found. The fractal exponent for pore distribution in Weglowicki sandstone was fitted using both stretched exponential and modified stretched exponential models. The results of both approaches are compared.

Liquid Phase Contained in Porous Rock as Observed by Proton Magnetic Relaxation