The H2O self-diffusion in hydrated fibrous zeolites (natrolite, mesolite, a
nd scolecite) at hydrostatic pressure up to 1.5 GPa was investigated using
nuclear magnetic resonance. It has been found that the effect of pressure o
n the diffusive mobility of water molecules arranged in the zeolite channel
s is different in various pressure-transmitting media. The compression in w
ater enhances molecular mobility corresponding to a negative activation Vol
ume of diffusion, which ranges from -5 to -12 cm(3) mol(-1) for the zeolite
s studied. The unusual pressure course of the activation process is shown t
o be associated with implanting exterior water molecules into the crystals
which results in an increase of the concentration of steady-state defects r
esponsible for the molecular diffusion. (C) 2001 Elsevier Science B.V. All
rights reserved.