E O Hercus 1936 Proc. Phys. Soc. 48 282 doi:10.1088/0959-5309/48/2/306
E O Hercus
Show affiliationsThe effect of dissolved air on the specific heat of water is calculated thermodynamically from the solubility data, for the case when no air is liberated, either completely or in the form of bubbles. It is shown that the specific heat of water saturated with air at 20° C. under normal atmospheric pressure exceeds that of air-free water by 6 × 10-6 cal./g.
Issue 2 (1 March 1936)
Received 19 August 1935
E O Hercus 1936 Proc. Phys. Soc. 48 282
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