Abstract
Tracer diffusion
coefficients of tritiated water (HTO) and 14C-labelled acetonitrile
have been measured at 298.15 K by the diaphragm cell method, for the whole
range of compositions of water+ acetonitrile binary mixtures. The composition
variation of (a) the deviation of D from additivity and (b) the product Dη, for each component, has been evaluated. The
variation of Dη is discussed in terms of the Naberukhin- Rogov structural
model for solutions of non-electrolytes in water. ��� The diffusion data have been used to test a
semiempirical relationship, between solution viscosity and self-diffusion
coefficients, due to Albright. For the composition region of 5-55 mole %
acetonitrile Albright's equation gives calculated viscosities which agree well
with observed values. The calculation fails to reproduce the observed variation
of viscosity for the composition region of 60-95 mole % acetonitrile.
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