Thermodynamics atmospheric pressure Question

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SUMMARY

The discussion focuses on calculating the increase in entropy for a liter of air heated at constant pressure until its volume doubles. The initial temperature is 300K, and the final temperature is determined to be 600K using the ideal gas law. The entropy change formula used is ΔS = Cp ln(Tf/Ti), where Cp for air is approximated as (7/2)R. The participants clarify that the number of moles (n) can be derived from the volume of air at standard temperature and pressure (STP).

PREREQUISITES
  • Understanding of the ideal gas law (PV=nRT)
  • Knowledge of entropy change calculations (ΔS = Cp ln(Tf/Ti))
  • Familiarity with specific heat capacities of gases (Cp for diatomic gases)
  • Basic principles of thermodynamics, particularly the second law
NEXT STEPS
  • Explore the derivation of the ideal gas law and its applications
  • Study the properties of diatomic gases and their specific heat capacities
  • Learn about entropy changes in various thermodynamic processes
  • Investigate the molar density of air at standard temperature and pressure (STP)
USEFUL FOR

This discussion is beneficial for students studying thermodynamics, particularly those tackling problems related to entropy changes in gases, as well as educators and professionals in physics and engineering fields.

benjibutton
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Homework Statement


A liter of air, initially at room temperature and atmospheric pressure, is heated at constant pressure until it doubles in volume. Calculate the increase in its entropy during this process.

so Ti= 300K, Volume which is 2Vi=Vf; Pressure is constant

Homework Equations


ΔS @constant pressure is = ∫Cp/T dT (where Ti -> Tf

The Attempt at a Solution


so since I don't know what T is but I know how the volume changes is there a way I can relate it? is it just PV=nkT so use V as an analog to gauge the proportional change in T? so would that give me something like Cp*Ln[2]?
 
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But you do know what T is - it's the temperature. You mean you are not told what the final temperature is?
Then - yes - you would need to draw information in from another source - the equation you are using for entropy change is for an ideal gas, so it seems reasonable to use the ideal gas law to relate temperature and volume. Unless you have some notes about how air behaves?

http://www.thebigger.com/chemistry/...anges-of-an-ideal-gas-in-different-processes/
 
Yeah, sorry; the final T is unknown. So do I write it as Ln[Tf/Ti]? where Tf= 2PVi/Nk ? how do I solve for N?
 
OK, I think I figured it out. I got it to be Tf=600K so it becomes 5/2*R*Ln(600K/300K)
 
benjibutton said:
OK, I think I figured it out. I got it to be Tf=600K so it becomes 5/2*R*Ln(600K/300K)
What happened to n? Your answer is for 1 mole, not 1 liter.
 
wouldn't n be the same for both sides of the ideal gas law, which would lead them to cancel out?
 
I also never had n, so I assumed you hold is constant, which would still give me the same result, since all other variables are held constant. Unless there's something else I'm missing.
 
At constant pressure $$\frac{PV_f=nRT_f}{PV_i=nRT_i}\implies \frac{V_f}{V_i} = \frac{T_f}{T_i}$$ ... it's a law that got named after someone.
It means you don't actually have to calculate the temperatures here if you know the volumes.

Of course you can also look up the molar density of air "at room temperature and atmospheric pressure".
 
benjibutton said:
wouldn't n be the same for both sides of the ideal gas law, which would lead them to cancel out?
Does it make sense to you that the change in entropy of 1 mole of gas is the same as the change in 1 liter? Your formula gave the change for 1 mole. So figure out how many moles in 1 liter of air at STP.

Your formula for ΔS = Cp ln(T2/T1) is correct. But Cp = ncp and you only have cp. BTW air is essentially a diatomic gas for which cp ~ (7/2)R.
 
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