The Thermodynamic Journey
Calculating Total Entropy Change
Imagine you are holding a block of ice at 273 K (0∘C). Your goal is to transform this solid block into superheated steam at 383 K (110∘C). This transformation doesn't happen in a single magical leap. It is a fascinating thermodynamic journey consisting of four distinct steps.
Because entropy (S) is a state function, the total change in entropy for this entire process is simply the sum of the entropy changes of each individual step. Let's break down this journey and calculate the entropy change at each milestone.
Step 1
Melting the Ice (Phase Change)
First, the ice must melt into liquid water. During this phase change, the temperature remains constant at 273 K. The heat added goes entirely into breaking the solid crystal lattice.
The formula for entropy change during a reversible phase transition at constant temperature is:
Substituting the given values:
ΔS1=273 K334 kJ kg−1=1.22 kJ kg−1K−1
Step 2
Heating the Water (Temperature Change)
Now we have liquid water at 273 K. We need to heat it up to its boiling point, 373 K. When the temperature of a substance changes without a phase change, the entropy change is calculated using its specific heat capacity (Cp):
Since we are given base-10 logarithm values, we must convert the natural logarithm (ln) to base-10 (log) by multiplying by 2.303:
ΔS2=4.2×2.303log(273373)
ΔS2=4.2×2.303(log373−log273)
ΔS2=4.2×2.303(2.572−2.436)=1.31 kJ kg−1K−1
Step 3
Boiling the Water (Phase Change)
At 373 K, the water begins to boil and turn into vapour. This is another phase change at a constant temperature. Notice how large the enthalpy of vaporization is compared to fusion; it takes a lot of energy to completely separate liquid molecules into a gas!
ΔS3=373 K2491 kJ kg−1=6.67 kJ kg−1K−1
Observe: This step produces the largest jump in entropy (6.67). This makes perfect physical sense because converting a relatively ordered liquid into a highly chaotic gas drastically increases the randomness (entropy) of the system.
Step 4
Heating the Vapour (Temperature Change)
Finally, we take our water vapour at 373 K and heat it further to 383 K. We use the temperature change formula again, but this time we must use the specific heat capacity of the vapour (2.0 kJ K−1kg−1).
ΔS4=2.0×2.303log(373383)
ΔS4=2.0×2.303(2.583−2.572)=0.05 kJ kg−1K−1
The Final Calculation
To find the total entropy change for the entire process, we simply sum up the entropy changes from all four steps:
ΔSTotal=ΔS1+ΔS2+ΔS3+ΔS4
ΔSTotal=1.22+1.31+6.67+0.05=9.25≈9.26 kJ kg−1K−1
By systematically breaking down a complex thermodynamic process into its fundamental atomic steps, we can easily navigate through the calculations and arrive at the correct answer!