When we talk about reversible melting of an ice cube, thermodynamic equilibrium is key. At thermodynamic equilibrium, there are no unbalanced forces within the system. For the ice cube, this equilibrium is reached when its temperature is equal to its melting point, which is 0°C (or 273.15 K). At this temperature, the ice cube can transition between solid and liquid phases without any net energy flow between it and the surrounding environment. Additionally, the pressure must be constant, typically at atmospheric pressure (1 atm or 101325 Pa).
In practice, this means the ice cube remains stable in its boundary conditions, ensuring a reversible process. Reversible processes are theoretically ideal, where the system changes state in an infinitely slow manner so as to maintain equilibrium.
- Temperature equals melting point: 0°C
- Constant pressure: 1 atm
- System changes occur without energy gradient
Achieving such a perfect state is more theoretical, but understanding it helps us grasp how melting can happen smoothly without abrupt energy exchange.