In physical processes, equilibrium is the state in which the forward and reverse processes proceed at equal rates, resulting in observable attributes of a system, such as temperature, pressure, or phase composition, staying constant across time.
In physical processes, equilibrium comes in the following primary forms:
When two things in thermal contact have the same temperature, this is known as thermal equilibrium.
When a system is in mechanical equilibrium, no net force is acting on it.
• Phase Equilibrium: When a substance’s phases coexist, such as in liquid-gas or solid-liquid equilibrium.
No, although energy exchange may still occur in certain situations, equilibrium usually happens in closed systems where no matter can enter or exit. Because of external interactions, open systems often undergo constant modification.
Phase equilibrium is strongly affected by temperature. For instance: • In solid-liquid equilibrium, the liquid phase often benefits from rising temperatures (e.g., ice melting to water).
• Higher temperatures accelerate evaporation, favoring the gas phase in liquid-gas equilibrium.
The system is dynamic even though it seems stable at equilibrium since the forward and reverse processes keep happening at the same pace, guaranteeing that the system’s characteristics don’t change overall.
Examples include: • A closed system with ice and water coexisting at 0°C (solid-liquid equilibrium).
• A sealed container containing water and its vapor at a steady temperature (liquid-gas equilibrium).
• Dry ice sublimation (solid-gas equilibrium) in a closed container.
Understanding equilibrium is essential for everyday applications, industrial processes, and natural occurrences. It facilitates the study of environmental cycles like the water cycle, clarifies phase transitions, and supports in the design of effective systems like freezers.