The surface tension, σ, of 97.8 percent deuterium oxide and of five more dilute mixtures with water has been compared with ordinary water by a modification of the capillary rise method. The results show that the relative surface tension is slightly less than that of pure water and is a linear function of the specific gravity. The data may be represented by the equation σ = 1 — 0.00501Δs, where Δs is the increase in specific gravity over ordinary water. By a slight extrapolation the surface tension of pure deuterium oxide at 25°C is estimated to be 0.999,46 of the surface tension of ordinary water at the same temperature.
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Jones et al. (1937) studied this question.
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