Abstract

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.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call