Question
When 1 mole of ice melts at 0°C and 1 atm, it absorbs 6.01 kJ of heat. Find , , and for this process. Then determine if ice will spontaneously melt at 263 K (−10°C), assuming and are temperature-independent.
Solution — Step by Step
At 273 K, melting is at equilibrium (both phases coexist), so and .
kJ/mol = +6010 J/mol (positive — heat absorbed).
J/(mol·K). Positive — entropy increases as ice melts.
Using the Gibbs equation:
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 : K. Above 273 K, (spontaneous melting). Below 273 K, (non-spontaneous melting; freezing is spontaneous).
Why This Works
The Gibbs equation is the master criterion for spontaneity at constant temperature and pressure. When , the process is spontaneous; when , the reverse process is spontaneous; at , the system is at equilibrium.
For phase transitions, and are roughly constant (we assume them so), and the transition temperature is the unique at which they balance: .
Memorize the four cases of and signs:
| Spontaneity | ||
|---|---|---|
| − | + | Always spontaneous |
| + | − | Never spontaneous |
| − | − | Spontaneous at low |
| + | + | Spontaneous at high (like melting) |
Ice melting falls in row 4: , , spontaneous above transition .
Alternative Method
Estimate using the formula directly without finding the transition temperature first. At any :
Plug : get J. Plug : get 0. Plug : get J. The sign change happens at 273 K.
Students confuse “spontaneous” with “fast.” Diamond → graphite is spontaneous at room temperature () but ridiculously slow. Spontaneity is a thermodynamic statement; rate is a kinetic one. Always separate the two.
Final answer: kJ/mol, J/(mol·K). At 263 K, J/mol > 0, so melting is non-spontaneous (ice stays ice).