Chemical Thermodynamics: Real-World Scenarios (8)

medium 3 min read

Question

When 1 mole of ice melts at 0°C and 1 atm, it absorbs 6.01 kJ of heat. Find ΔH\Delta H, ΔS\Delta S, and ΔG\Delta G for this process. Then determine if ice will spontaneously melt at 263 K (−10°C), assuming ΔH\Delta H and ΔS\Delta S are temperature-independent.

Solution — Step by Step

At 273 K, melting is at equilibrium (both phases coexist), so ΔG=0\Delta G = 0 and TΔS=ΔHT \Delta S = \Delta H.

ΔH=+6.01\Delta H = +6.01 kJ/mol = +6010 J/mol (positive — heat absorbed).

ΔS=ΔH/T=6010/27322.0\Delta S = \Delta H / T = 6010 / 273 \approx 22.0 J/(mol·K). Positive — entropy increases as ice melts.

Using the Gibbs equation:

ΔG=ΔHTΔS=6010(263)(22.0)=60105786=+224 J/mol\Delta G = \Delta H - T \Delta S = 6010 - (263)(22.0) = 6010 - 5786 = +224 \text{ J/mol}

ΔG>0\Delta G > 0 at 263 K (= −10°C), so melting is non-spontaneous at this temperature. Ice will not spontaneously melt at −10°C — instead, water freezes.

Set ΔG=0\Delta G = 0: T=ΔH/ΔS=6010/22.0273T = \Delta H / \Delta S = 6010 / 22.0 \approx 273 K. Above 273 K, ΔG<0\Delta G < 0 (spontaneous melting). Below 273 K, ΔG>0\Delta G > 0 (non-spontaneous melting; freezing is spontaneous).

Why This Works

The Gibbs equation ΔG=ΔHTΔS\Delta G = \Delta H - T \Delta S is the master criterion for spontaneity at constant temperature and pressure. When ΔG<0\Delta G < 0, the process is spontaneous; when ΔG>0\Delta G > 0, the reverse process is spontaneous; at ΔG=0\Delta G = 0, the system is at equilibrium.

For phase transitions, ΔH\Delta H and ΔS\Delta S are roughly constant (we assume them so), and the transition temperature is the unique TT at which they balance: Ttransition=ΔH/ΔST_{\text{transition}} = \Delta H / \Delta S.

Memorize the four cases of ΔH\Delta H and ΔS\Delta S signs:

ΔH\Delta HΔS\Delta SSpontaneity
+Always spontaneous
+Never spontaneous
Spontaneous at low TT
++Spontaneous at high TT (like melting)

Ice melting falls in row 4: ΔH>0\Delta H > 0, ΔS>0\Delta S > 0, spontaneous above transition TT.

Alternative Method

Estimate ΔG\Delta G using the formula directly without finding the transition temperature first. At any TT:

ΔG(T)=ΔHTΔS\Delta G(T) = \Delta H - T \Delta S

Plug T=263T = 263: get +224+224 J. Plug T=273T = 273: get 0. Plug T=283T = 283: get 220-220 J. The sign change happens at 273 K.

Students confuse “spontaneous” with “fast.” Diamond → graphite is spontaneous at room temperature (ΔG<0\Delta G < 0) but ridiculously slow. Spontaneity is a thermodynamic statement; rate is a kinetic one. Always separate the two.

Final answer: ΔH=+6.01\Delta H = +6.01 kJ/mol, ΔS=+22.0\Delta S = +22.0 J/(mol·K). At 263 K, ΔG=+224\Delta G = +224 J/mol > 0, so melting is non-spontaneous (ice stays ice).

Want to master this topic?

Read the complete guide with more examples and exam tips.

Go to full topic guide →

Try These Next