The Beauty of Thermodynamics
Thermodynamics is the study of energy in transit. It governs everything from the engines in our cars to the beating of our hearts. In this epic problem, we are tasked with finding the change in internal energy (ΔU) for four completely different physical systems. It is like a grand tour of the First Law of Thermodynamics!
Process I
The Boiling Cauldron
Imagine a tiny amount of water, just 10−3 kg (or 1 gram), sitting at its boiling point of 100∘C. We are pumping heat into it to convert it entirely into steam.
First, how much heat are we actually supplying? We use the latent heat of vaporization. The heat supplied is ΔQ=mL. Plugging in the values, we get ΔQ=10−3×2250 kJ/kg=2.25 kJ.
But wait, the steam takes up much more space than the liquid water! It expands against the atmospheric pressure of 105 Pa. This means the system is doing work on the universe. The work done is ΔW=PΔV. The volume changes from a minuscule 10−6 m3 to 10−3 m3.
Calculating this, ΔW=105×(10−3−10−6)≈100 J=0.1 kJ.
According to the First Law of Thermodynamics, ΔU=ΔQ−ΔW. The internal energy increases by 2.25−0.1=2.15 kJ. The closest match is 2 kJ.
Process II
The Expanding Diatomic Gas
Next, we have 0.2 moles of a rigid diatomic gas expanding at constant pressure. The volume triples from V to 3V.
Because the pressure is constant, Charles's Law tells us that the temperature must also triple! The initial temperature is 500 K, so the final temperature becomes 1500 K. The change in temperature is a massive ΔT=1000 K.
For a rigid diatomic gas, the molar heat capacity at constant volume is CV=25R.
Even though the process is isobaric, the change in internal energy for an ideal gas is always given by ΔU=nCVΔT.
Substituting our values: ΔU=0.2×(25×8.0)×1000=4000 J=4 kJ.
Process III
The Swift Adiabatic Crush
Now, imagine a monatomic gas being compressed so rapidly that no heat can escape. This is an adiabatic process (ΔQ=0).
The volume is crushed from V to V/8. To find the new pressure, we use the adiabatic relation P1V1γ=P2V2γ. For a monatomic gas, γ=35.
P2=P1(V2V1)γ=2 kPa×(8)5/3. Since 8 is 23, 85/3 is simply 25=32. So, the final pressure shoots up to 64 kPa!
The change in internal energy is exactly the negative of the work done: ΔU=γ−1P2V2−P1V1.
Plugging in the pressures and volumes, we get ΔU=23(64×241−2×31)=23(38−32)=3 kJ.
Process IV
The Vibrating Molecules
Finally, we encounter a diatomic gas that isn't rigid. Its molecules are vibrating! This adds 2 extra degrees of freedom, bringing the total to f=7.
This means CV=27R and CP=29R.
We are told that 9 kJ of heat is supplied at constant pressure. So, ΔQ=nCPΔT=9 kJ.
We need ΔU, which is nCVΔT. Notice the beautiful shortcut here: the ratio ΔQΔU is simply CPCV=97.
Therefore, ΔU=97×9 kJ=7 kJ.
The Grand Conclusion
We have successfully navigated four distinct thermodynamic landscapes. By trusting the First Law and understanding the degrees of freedom, we matched every process perfectly. This is the true power of physics!