BRIDGMAN. — THERMODYNAMIC PROPERTIES OF WATER. 



341 



at 20°, although it has not yet risen to the vakie at 0°. ]n achhtion 

 to the abnormality at low pressures, the curve shows also a slight 



TABLE V. 



COMPRESSIRILITY OP H2O. 



abnormality at the higher pressures in the neighborhood of 6500 kgm. 

 Here the compressibility at 20° rises and at the melting point of ice 

 VI, it has become higher than the compressibility at 80°. The thermal 

 dilatation shows abnormality in the same locality; it would seem to be 



