Thermodynamic process

A transformation that carries a thermodynamic system between states along a specified path of interactions with its surroundings.
Thermodynamic process

A thermodynamic process is a time-ordered transformation of a driven by interactions with the across a . Depending on whether the system is , , or , the process may involve exchange of energy (as heat and/or work) and possibly matter.

When the system is (at least approximately) in throughout, the process can be represented as a continuous path through parameterized by (e.g., temperature, pressure, volume, particle number). In general, a process may pass through nonequilibrium configurations, in which case only the endpoints may be equilibrium states with well-defined macroscopic state variables.

Physical interpretation

A process is “what you do to the system” (or “what happens to it”)—compressing a gas, heating it in contact with a reservoir, letting it expand against an external pressure, mixing components, or allowing chemical change—specified by the constraints and how external controls vary in time. The same initial and final equilibrium states can often be connected by many different processes; the distinction matters because some quantities depend on the path.

Key structural distinctions

A thermodynamic process separates naturally into:

  • State changes described by (quantities determined solely by the state). For any state function XX, the change ΔX\Delta X depends only on the initial and final equilibrium states, not on the process used to connect them.
  • Transfers described by (quantities defined through the process history). In particular, heat and work are represented by the δQ\delta Q and the δW\delta W, whose integrals generally depend on the path.

A standard differential statement of the is

dU=δQδW, dU = \delta Q - \delta W,

where UU is the and the sign of δW\delta W follows the chosen .

Common refinements

Important special classes of thermodynamic process include the (intermediate states remain arbitrarily close to equilibrium), the (idealized, no dissipation and no net change to system+surroundings upon reversal), the (realistic, dissipative, entropy-producing), and the (returns to the initial state).