OP
will_tekkie
Contributor
donacheson:As I recall, most second stages operate with an input pressure about 100 psi more than ambient, so a calculation can be made of a typical adiabatic temperature drop in a second stage. Since T1/T2=(P1/P2)^0.286 (both teperatures and pressures are absolute), the adiabatic temperature drop in 33 feet of 68F sea water would be about 180F and in 100 feet of 68F sea water, about 130F. Obviously, we don't breath air chilled that much, so the transfer of heat within the second stage is very important - and difficult to estimate theoretically, thus requiring measurement.
i´m agree again...obviously a adiabatic expansion is not according to the actual process (as we said at the beginning of the threats) so if you read the article above you will see some lab tests made in regulators that can help a lot...real temps are shown...therefore as we made above the heat transfer can be estimated from the presures and temps measured in the cases presented...of course all values are rough and the real ones should depends of each case, there are too many factors involved...a dive in the sea is not the same than a reg tested in a lab.