Contribution .Vo. 980 f r o m the Institute of Marine Sciences, Unisersity of M i a m i , M i a m i , Florida (Received April 12, 1968) 331 49The relative viscosity of water has been measured with high precision in the range from 8 to 70" using a modified Cannon-Ubbelohde suspended-meniscus, dilution viscometer with a semiautomatic, optical viscometer reader. Measurements were made at, 1' intervals with a relative precision of about 0.0017,. The apparent energy of activation for viscous flow of water was calculated from these data. The result is given by an equation of the form AE* = A -+-BT + CT2 + DTa + ET4. The root-mean-square deviation from this expression was 3.7 cal/g-mol (Le,) approximately 0.1% in AB!*). The resu1t)s obtained did not reveal any abrupt changes, at discrete temperatures, in the observed energy of act,ivation values. The suggestion is offered that some of the thermal anomalies ("kiiiks") which have been reported in bulk properties of water may have arisen from structural transitions in ordered water structures near interfaces.

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An apparatus is described for the measurement of the isothermal compressibility of liquids at pressures up to 50 atm. and temperatures to 60°C. The apparatus has been used to measure

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