Thermodynamic equilibrium denotes a state where a system's macroscopic properties remain constant over time. This state is achieved when a system balances its energy and matter exchange with its surroundings and internal components. Three primary equilibrium types define these aspects:
• Mechanical Equilibrium: No net forces act on the system or its parts, implying no pressure gradients. In closed systems, pressure is uniform.
• Chemical Equilibrium: The system's chemical composition remains unchanged; the net rate of all chemical reactions is zero, preventing further net conversion between reactants and products.
• Thermal Equilibrium: The system's temperature is uniform internally and matches its surroundings, eliminating further net heat exchange.
Achieving full thermodynamic equilibrium requires satisfying all three conditions concurrently.