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merronys
7th Mar 2002, 22:00
I know it's Boyle's law and all that, but I can't find the factors I need for this one.... .. .What volume would a cubic metre of air at sea-level in ISA occupy if temperature is raised by 1 degree celcius?

bluskis
7th Mar 2002, 23:47
Volume would be [273+16]/[273+15]cu m, ignoring any change in pressure.That is the volume ratio is proportional to the absolute T ratio.

Chris2
8th Mar 2002, 12:28
Is this a question which appears in JAA atpl exams ??????

Genghis the Engineer
8th Mar 2002, 13:09
Anybody noticed that there are people with other interests than passing ATPL exams? Some of them are even aviation professionals and members of Pprune.. .. .G

merronys
8th Mar 2002, 13:30
Thanks bluskis.. .. .No - it's not an exam question, I am just trying to knock up a simplistic atmospheric simulation to help drum in some met. into my addled brain <img border="0" title="" alt="[Roll Eyes]" src="rolleyes.gif" /> . (I suppose that's what you get when us IT-types try to become flying types...)

Genghis the Engineer
8th Mar 2002, 16:04
For a computer model, you'd be best off using the basic ISA derivative equations for density, pressure and temperature. The relationships are exponential up to the tropopause, then - well - otherwise.. .. .If you want basic proofs, any undergraduate aerodynamics textbook will give you that. "Aerodynamics for Engineering Students" by Houghton+1 is the best known, although I prefer "Aerodynamics" by Clancy. It's pretty straightforward to model the lower atmosphere from first principles.. .. .If you are looking for small changes, then relative density = relative pressure divided by relative temperature - always working in absolute (Kelvin or Rankine) temperature, not relative (Celcius or Farenheit).. .. .G