Air pressure - density -temperature at 10,000 meters

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Discussion Overview

The discussion revolves around the air pressure, density, and temperature at an altitude of 10,000 meters, particularly in the context of airplane cabins. Participants explore theoretical calculations and assumptions related to the ideal gas law, the behavior of air at high altitudes, and the effects of pressurization and air conditioning.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant notes the air temperature at 10,000 meters is -35º C and mentions that cabin temperatures are maintained by air conditioning rather than heating.
  • Another participant suggests that the ideal gas equation is applicable but points out that significant assumptions must be made due to insufficient information.
  • A participant shares a formula provided by their teacher, which includes a specific air density value of 1.29 kg/m3, but questions its validity at higher altitudes where density decreases.
  • Calculations presented by a participant yield a density of 0.38696 kg/m3 and a pressure of 63403 Pa, but they express uncertainty about the correctness of their results.
  • One participant emphasizes the importance of considering pressurization in an airplane, suggesting that the air density used in calculations should reflect conditions inside the cabin rather than at sea level.
  • Another participant argues that it is impossible to calculate the outside air pressure without knowing how much the air conditioner has cooled the air and recommends using external resources for pressure and density data.

Areas of Agreement / Disagreement

Participants express differing views on the validity of using a constant air density value at high altitudes, the applicability of the ideal gas law, and the impact of pressurization on temperature and pressure calculations. The discussion remains unresolved with multiple competing perspectives.

Contextual Notes

Participants highlight limitations related to assumptions about air density at altitude, the effects of pressurization, and the need for additional information to accurately calculate pressure and temperature.

Sherry
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The air temperature at an altitude of 10,000 meters is a chilling
-35º C. Cabin temperatures in airplanes flying at this altitude are comfortable because of air conditioners rather than heaters. A.) Find the pressure at 10,000 m and B) Find the temperature of the air before the air conditioner cools it off.
 
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Ideal gas equation (not enough information is given though - some big assumptions need to be made).
 
This was a question the teacher gave us to think about over the weekend.

The only clue he gave us in class is:
101325 Pa = (1.29 kg/m3)(h) where h = 8015 meters.

He told us to use air density 1.29 kg/m3 but that does not make sense because dry air at sea level is 1.29 kg/m3 but as altitude increases, the density drops dramatically.


I found other formulas and worked the problem this way:

Where: D = density, kg/m3
P = pressure, Pascals
R = gas constant , J/(kg*degK) = 287.05 for dry air
T = temperature, degK = deg C + 273.15


D = P/R*T D = 26436/(287.05 * 238) D = 0.38696 kg/m3
P = 101325-egh P = 101325-(0.38696)(9.80)(10000) P = 63403 Pa
P = Po(Tf/To) 101325 = 63403(Tf /238) Tf = 380 K = 107 C

I am just not sure that it is right.
 
Last edited:
Originally posted by Sherry
He told us to use air density 1.29 kg/m3 but that does not make sense because dry air at sea level is 1.29 kg/m3 but as altitude increases, the density drops dramatically.

But not inside a pressurised airliner. I believe that is the key to resolving this question.
 
Correct, but he wants us to find the pressure outside of the plane at 10,000 meters as well as the temperature of the air as it is being pressurized but before the plane's air conditioner cools it off.
 
You can't calculate the air pressure outside the plane from the info given because you don't know how much the air conditioner has cooled the air. Find the pressure and density through http://www.npl.co.uk/pressure/faqs/atmosaltitude.html chart (if it isn't specific enough, calculate it by fitting a line to the graph) and calculate the temperature of the air once its been pressurized using the ideal gas equation.
 

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