In recent years, there has been an increasing interest in 1H nuclear magnetic resonance (NMR) relaxometry to obtain information on the hydration and porosity of cement stone. By spin-spin (T2), spin-lattice (T1), and combined relaxation studies, new insights were gained on liquid and crystal bound water as well as pore water exchange. A conversion of relaxation times to pore sizes has been developed and shown to give consistent results. In this study, we use single-sided 1H NMR to obtain two-dimensional T1-T2 relaxation distributions on systematically varied cement stone samples as well as hydrated and solid cement phases. Results show a richness in features beyond past studies and are interpreted qualitatively in terms of water found in chemically different pore environments. Both T1 and T2 surface relaxivity of calcium silicate surrounded liquid water linearly correlate with the cement's Fe2O3 content. Results are discussed based on a theory of interacting surface relaxation mechanisms.
Read full abstract