Question: Entropy production by irreversible work. One mole of air at 2 7 C and 5 0 0 kPa in a 1 0 0 kPa atmosphere

Entropy production by irreversible work. One mole of air at 27C and 500kPa in a 100kPa atmosphere expands to 100kPa by free expansion in a piston-cylinder device. After the expansion, the air in the device reaches an equilibrium temperature by transferring heat from the surrounding air, which has a temperature of 27C. Calculate the increase in entropy associated with this process.
(a) Define the system to be the gas in the piston-cylinder and the surroundings to be the atmosphere around the system. Draw a schematic of the process showing state 1(500kPa) and state 2(100kPa). Label it as completely as you can.
(b) Use the equation, Sgen=Sproc+Ssur. I will call this "the sum of entropies approach". You can calculate Sproc directly from the given information.
(c) What is the path over which you calculate the entropy change of the system? Read the problem, what are the initial and final states? What reversible path could you use to connect them? It is a process in which an ideal gas expands from 500kPa to 100 kPa and the final and initial temperatures are the same.
(d) Since you take a reversible path you can use one of the S equations I derived, or one from the equation sheet, or from the text. Typical reversible paths include isothermal expansion compression adiabatic expansion/compression, isobaric expansion/compression isobaric heating/cooling, isochoric heating/cooling. You couldalso directly evaluate dQT|rev
(e) Calculate S??(proc). This is straight-forward. You should find it to be 13.38JK.
(f) For the sum of entropies approach, you need to find S??(sur). You find this by applying the energy balance to the system to find Q transferred from the surroundings. For this isothermal process, what is the energv balance on the svstem?
(g) You should see the the heat transferred (to the system) is the negative of the work (done by the system on the surroundings, the atmosphere). Unfortunately the work calculation is tricky and a bit confusing because we cannot calculate the work by the system directly. This is because we don't know the path. The process is irreversible, and the isothermal expansion equation that we would like to use is invalid. However, we can calculate work on the surroundings. It is an isobaric process atmospheric pressure is constant. Once we know that we recognize Wsys=-Wsur.
(h) Using the isobaric work formula show that Wsur=Psur(V2sur}
{:V1sur). We don't know Vsur but we know Vsur=-Vsys and
PV=RT. Put this together with the energy balance and show
Q??(sys)=nRT(PatmP2-PatmP1)
(i) Evaluate this to find the heat transfer of 1995J, positive because
it goes into the system.
(j) Since any heat that crosses into the system has to come from the
surroundings, we know Qsur and since it is heat lost from the
surrounding it must be negative.
(k) What is T for the surface that heat transfers over? Use that and
above to find Ssur=-6.65JK.
(l) What is Sgen?
(m) As an alternative way to find Sgen,, write down the integrated
closed-system entropy balance and use the numbers you calcu-
lated above for Ssys and Qsys to calculate Sgen.
(n) You also might consider an alternative approach to compute Qsys.
You could treat the surrounding as a system of its own and per-
form an energy balance on the surroundings. It will also show
Qsys=-Wsys where the work is computed as above, using con-
stant P expansion.
 Entropy production by irreversible work. One mole of air at 27C

Step by Step Solution

There are 3 Steps involved in it

1 Expert Approved Answer
Step: 1 Unlock blur-text-image
Question Has Been Solved by an Expert!

Get step-by-step solutions from verified subject matter experts

Step: 2 Unlock
Step: 3 Unlock

Students Have Also Explored These Related Chemical Engineering Questions!