Clausius inequality

Integral inequality for heat exchange that quantifies irreversibility and leads to the definition of entropy.
Clausius inequality

Consider a in which a system exchanges heat δQ\delta Q with its surroundings (see ). Let TbT_{\mathrm{b}} denote the at which each heat element crosses the system boundary (e.g., the temperature of a supplying that heat), understood on the . The Clausius inequality states that

δQTb0. \oint \frac{\delta Q}{T_{\mathrm{b}}}\le 0.

Equality holds if and only if the cycle is ; strict inequality indicates a genuinely cycle.

A useful special case is a cycle exchanging finite heats QiQ_i with reservoirs at fixed temperatures TiT_i:

iQiTi0. \sum_i \frac{Q_i}{T_i}\le 0.

Physical interpretation

The inequality expresses the content of the in a form that directly compares heat transfers at different temperatures: heat exchanged at lower temperature carries a larger “entropy weight” δQ/T\delta Q/T. The strictness of the inequality measures how much irreversibility is present in the cycle.

Key relations

  • Entropy as a state function. For a reversible process between equilibrium states AA and BB, the integral of δQ/Tb\delta Q/T_{\mathrm{b}} is path-independent. This motivates defining the change by

    S(B)S(A)=ABδQrevT, S(B)-S(A)=\int_A^B \frac{\delta Q_{\mathrm{rev}}}{T},

    where the subscript “rev” emphasizes evaluation along a reversible path (so the boundary and system temperatures coincide).

  • Inequality for general processes. For any process between equilibrium states,

    S(B)S(A)ABδQTb, S(B)-S(A)\ge \int_A^B \frac{\delta Q}{T_{\mathrm{b}}},

    with equality only in the reversible limit.

  • Entropy production form. Writing

    ΔSδQTb=Sgen, \Delta S - \int \frac{\delta Q}{T_{\mathrm{b}}} = S_{\mathrm{gen}},

    the Clausius inequality is equivalent to Sgen0S_{\mathrm{gen}}\ge 0.

  • Adiabatic implication. If the system is thermally insulated by an so that δQ=0\delta Q=0, then ΔS0\Delta S\ge 0 for a closed system, with equality only for a reversible adiabatic (isentropic) change.