Rs. Chen et al., EFFECTS OF HYDROSTATIC-PRESSURE ON PROTON AND DEUTERON MAGNETIC-RESONANCE OF WATER IN NATURAL ROCK AND ARTIFICIAL POROUS-MEDIA, Journal of magnetic resonance. Series A, 110(1), 1994, pp. 77-81
The effect of pressure on the NMR longitudinal relaxation of D2O and H
2O confined to the interstices of natural and artificial porous media
is reported. Magnetization decays of fluid protons in natural porous m
edia are known to be dominated by interactions between water molecules
and the surface of the solid matrix. These decays are characterized b
y broad distributions of relaxation times. In some materials there is
no pressure dependence of the proton relaxation time distribution, whi
le in other materials minor effects are noted. The NMR relaxation of d
euterium in D2O is dominated by intramolecular effects. Assuming that
the enhancement of relaxation at the surface is relatively independent
of surface composition, one can estimate a surface-to-pore-volume rat
io. The NMR S/V is more useful than that measured by conventional meth
ods. The pressure dependence of D2O relaxation in porous media follows
that of the bulk liquid. (C) 1994 Academic Press, Inc.