Abstract
Abstract The usual approach utilising the Van't Hoff factor (or the mean ionic activity coefficient) cannot be applied to the thermodynamic equilibrium equation describing the growth of a molecular solution droplet formed in a water vapor atmosphere. A new semi‐empirical formula applicable to sustances which do not dissociate into ions in water is developed. As an example, the nucleus activity formulation for very hygroscopic organic nuclei ‐ such as dimethylsulfoxide ‐ is discussed. This substance is used for studying the possibility to disperse a dense fog of limited extent.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
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
