SHEAR VISCOSITY AND SELF-DIFFUSION EVIDENCE FOR HIGH-CONCENTRATIONS OF HYDROGEN-BONDED CLATHRATE-LIKE STRUCTURES IN VERY HIGHLY SUPERCOOLEDLIQUID WATER
Ge. Walrafen et Yc. Chu, SHEAR VISCOSITY AND SELF-DIFFUSION EVIDENCE FOR HIGH-CONCENTRATIONS OF HYDROGEN-BONDED CLATHRATE-LIKE STRUCTURES IN VERY HIGHLY SUPERCOOLEDLIQUID WATER, Journal of physical chemistry, 99(26), 1995, pp. 10635-10643
Activation energies from shear viscosity and self-diffusion of highly
supercooled liquid water rise very rapidly with decreasing temperature
at 1 atm and approach approximate to 70 kJ/mol, or more, at 228 K. Th
ese high values may result because the flow of H2O molecules is impede
d by passage through hydrogen-bonded pentagonal rings whose opening ra
dius is approximate to 0.4 Angstrom, smaller than the van der Waals ra
dius of H2O. Two principal effects may contribute to the overall energ
etics: (1) breakage of hydrogen bonds around a given H2O molecule; and
then, only if no opportunity exists for free diffusion through hexago
nal or larger rings in the immediate vicinity of the freed H2O molecul
e, (2) impeded, highly endothermic diffusion of that H2O molecule thro
ugh a hydrogen-bonded pentagon, by forced ring expansion, followed by
rebinding of the H2O. Large negative activation volumes are also indic
ated from 273 to 228 K and 1 atm. These negative volumes may arise fro
m activated filling of voids in bulky, clathrate-like, polyhedral stru
ctures. A model for the diffusional process is described.