“…Thus, the heat addition is proportional to evolved wetness which can be obtained by evaluation of the socalled nucleation-growth integrals [Dobbins, 1983] as will be discussed below. The Rayleigh flow relationships ( [Cengel and Boles [2008], [Dobbins, 1983], [Ding et al, 2013]) are such that a downstream state (e.g. state 'n') can be determined from an upstream state (idealized state 'a' in this case) and a known heat addition between states.…”