The world of thermodynamics is filled with fascinating cycles, and this problem is a perfect example of how different thermodynamic processes weave together to form a complete story. We are given a p-T diagram for two moles of an ideal monoatomic gas undergoing a cyclic process ABCA. Our mission? To decode the work done and heat exchanged in each leg of the journey.
Let's take a deep breath and break this down step-by-step.
Analyzing the Setup
Before we jump into any calculations, we must orient ourselves by identifying the exact coordinates of our states on the p-T diagram. The problem gives us T1=300 K.
Looking at the graph, we can pinpoint the states:
- State A: The temperature is 2T1=600 K and the pressure is p1.
- State B: The temperature drops to T1=300 K while the pressure rises to 2p1.
- State C: The temperature goes back up to 2T1=600 K and the pressure remains at 2p1.
We are also told that the gas is monoatomic. This is a crucial piece of intel! It tells us that the molar heat capacity at constant volume is CV=23R, and at constant pressure, it is Cp=25R.
The Master Equation for Process AB
The path from A to B is not your standard isobaric or isothermal process. We are given a unique constraint: pT=constant.
How do we find the work done, W=∫pdV, when the relationship is between p and T? We need to express pdV entirely in terms of dT. Let's use the power of calculus!
Differentiating the given condition
pT=constant using the product rule, we get:
pdT+Tdp=0⟹Tdp=−pdT
Now, let's bring in the trusty ideal gas equation,
pV=nRT. Differentiating this gives:
pdV+Vdp=nRdT
We need to eliminate the
Vdp term. From the ideal gas law, we know
V=pnRT. Substituting this into our differential equation:
pdV+(pnRT)dp=nRdT
Now, substitute
Tdp=−pdT into the equation:
pdV+pnR(−pdT)=nRdT
Moving the terms around, we arrive at a beautifully simple relation:
pdV=2nRdT
Calculating Work and Heat for Process AB
Now that we have
pdV=2nRdT, finding the work done is a breeze. We just integrate from
TA to
TB:
WAB=∫TATB2nRdT=2nR(TB−TA)
Substitute the known values (
n=2,
TA=600 K,
TB=300 K):
WAB=2(2)R(300−600)=−1200R
The negative sign indicates that work is done on the gas (compression).
Next, we need the heat exchanged,
QAB. According to the First Law of Thermodynamics,
Q=W+ΔU. Let's find the change in internal energy:
ΔUAB=nCV(TB−TA)=2(23R)(300−600)=−900R
Adding them up:
QAB=−1200R−900R=−2100R
Heat is released by the gas during this process.
The Isobaric Journey
Process BC
Process B to C is a horizontal line on the p-T diagram, which means the pressure is constant. This is an isobaric process!
For an isobaric process, the heat exchanged is directly calculated using
Cp:
QBC=nCp(TC−TB)
Substitute the values (
TC=600 K,
TB=300 K):
QBC=2(25R)(600−300)=5R(300)=1500R
Since the result is positive, heat is absorbed by the gas.
The Isothermal Finale
Process CA
Finally, process C to A is a vertical line on the p-T diagram. The temperature is constant at 600 K, making this an isothermal process.
In an isothermal process, the change in internal energy is zero (
ΔUCA=0). Therefore, the heat exchanged is exactly equal to the work done:
QCA=WCA=nRTCln(VCVA)
Since
pAVA=pCVC (Boyle's Law), we can replace the volume ratio with the pressure ratio:
QCA=nRTCln(pApC)
Substitute the values (
pC=2p1,
pA=p1):
QCA=2R(600)ln(p12p1)=1200Rln(2)
Given that
ln(2)≈0.693:
QCA=1200R(0.693)=831.6R
Heat is absorbed by the gas as it expands back to its original state.
Conclusion
We have successfully navigated the entire cycle! By breaking down the p-T diagram and applying the First Law of Thermodynamics to each specific path, we unlocked the secrets of the gas's journey. Remember, the key to mastering thermodynamics is to stay calm, identify the constraints of each process, and trust your fundamental equations. Keep practicing, and these cycles will become second nature!