Overview
Internal energy, usually denoted by U (or sometimes E), is the total microscopic energy contained within a thermodynamic system. It comprises the kinetic energy of particles (translational, rotational and vibrational motion) and the potential energy associated with molecular interactions, chemical bonds and electronic configurations. Internal energy excludes bulk translational kinetic energy of the system as a whole and macroscopic external potential energy due to fields acting on the entire body.
Key characteristics
Internal energy is a state function: its value depends only on the thermodynamic state of the system, not on the history of how that state was reached. It is an extensive quantity (proportional to the system size); the corresponding intensive quantity is specific internal energy (energy per unit mass). The SI unit is the joule, although calories remain in common use for heat-related contexts.
In classical thermodynamics the first law expresses energy conservation for closed systems in terms of internal energy: the change in internal energy equals heat added to the system minus work done by the system. For many idealized models, such as an ideal monatomic gas, the internal energy depends primarily on temperature. For real substances, U also varies with volume and composition because of intermolecular forces and chemical bonding.
Microscopic origin and statistical view
From a microscopic perspective, internal energy is the expectation value of the system's Hamiltonian over its microscopic states. It therefore includes contributions from molecular motions, vibrational modes, electron energies in atoms and solids, and, where relevant, radiation energy (for example, blackbody radiation confined in a cavity). In solids and metals, free electron energy and lattice vibrations (phonons) are significant parts of U.
Applications and importance
Internal energy underlies heat capacity, phase transitions, chemical reaction energetics, and the performance of heat engines and refrigerators. Changes in internal energy are measured by calorimetry and inferred in many processes using thermodynamic relations. Enthalpy, another common thermodynamic quantity, is defined as H = U + pV and is useful for processes at constant pressure.
Equilibrium, constraints and notable facts
At equilibrium and for a closed system, thermodynamic potentials take extremal values under fixed constraints: at constant entropy and volume, the internal energy is minimized. Distinguishing internal energy from kinetic or potential energy associated with the system as a whole is important when formulating conservation laws. Radiation and electronic excitation can contribute significantly to U at high temperatures.
History and conceptual development
The concept of internal energy developed in the 19th century as scientists such as James Prescott Joule, Julius Robert Mayer and others clarified the equivalence of heat and mechanical work and established energy conservation for thermal processes. That work led to the formulation of the first law of thermodynamics and to modern treatments that connect macroscopic thermodynamic quantities to microscopic statistical mechanics.
Related topics and references
- Thermodynamics overview
- Thermodynamic system definitions
- System boundaries and control volumes
- Kinetic energy in molecules
- Molecular motion types
- Rotational degrees of freedom
- Vibrational modes
- Intermolecular potential energy
- Electric interactions in matter
- Atomic and electronic structure
- Crystalline solids and lattices
- Energy units and conversions
- Chemical bond energy
- Conduction electrons in metals
- Properties of metals
- Thermodynamic potentials
- Closed and open systems
- Entropy and thermodynamic constraints
- Electromagnetic and radiation energy
- State functions
- Joule and the SI system
- Calorie as a historical unit
- Heat and calorimetry