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Review

1. Checklist of Key Concepts

Section 4.1: Entropy

  1. Exothermicity Does Not Guarantee Spontaneity

    • ΔH<0\Delta H < 0 (exothermic) often favors spontaneity but does not determine it. Counter-example: mixing of two ideal gases is spontaneous even though ΔH=0\Delta H = 0.

    • A complete account of directionality requires entropy.

  2. Definition of Entropy

    • Entropy is a state function defined by

    dS=δqrevT.dS = \frac{\delta q_{\mathrm{rev}}}{T}.
    • The finite change between states AA and BB is ΔS=∫ABδqrev/T\Delta S = \int_A^B \delta q_{\mathrm{rev}}/T, evaluated along any reversible path connecting those states.

  3. Exactness of δqrev/T\delta q_{\mathrm{rev}}/T

    • δqrev\delta q_{\mathrm{rev}} is inexact, but dividing by TT produces an exact differential. Verification for an ideal gas: the cross-derivative test on CV/TC_V/T and NkB/VNk_{\mathrm{B}}/V gives matching mixed partials (both zero).

  4. Entropy of Irreversible Processes

    • Because SS is a state function, ΔS\Delta S depends only on the endpoints. To compute ΔS\Delta S for an irreversible process, find any convenient reversible path between the same initial and final states and integrate δqrev/T\delta q_{\mathrm{rev}}/T along that path.

  5. Fundamental Thermodynamic Relation

    • Combining δqrev=T dS\delta q_{\mathrm{rev}} = T\,dS and δwrev=−P dV\delta w_{\mathrm{rev}} = -P\,dV in the First Law:

    dU=T dS−P dV.dU = T\,dS - P\,dV.
    • The natural variables of UU are SS and VV. This relation replaces two inexact differentials (δq\delta q, δw\delta w) with three exact ones (dUdU, dSdS, dVdV).


Section 4.2: Carnot Cycle

  1. Structure of the Carnot Cycle

    • A fully reversible cycle operating between a hot reservoir (ThotT_{\mathrm{hot}}) and a cold reservoir (TcoldT_{\mathrm{cold}}), consisting of four steps:

      • A→BA \to B: reversible isothermal expansion at ThotT_{\mathrm{hot}} (system absorbs heat qAB>0q_{AB} > 0).

      • B→CB \to C: reversible adiabatic expansion (system cools, q=0q = 0).

      • C→DC \to D: reversible isothermal compression at TcoldT_{\mathrm{cold}} (system releases heat qCD<0q_{CD} < 0).

      • D→AD \to A: reversible adiabatic compression (system warms, q=0q = 0).

  2. Entropy Bookkeeping Around the Cycle

    • Adiabatic steps are isentropic: ΔSBC=ΔSDA=0\Delta S_{BC} = \Delta S_{DA} = 0.

    • Isothermal steps carry entropy: ΔSAB=qAB/Thot\Delta S_{AB} = q_{AB}/T_{\mathrm{hot}}, ΔSCD=qCD/Tcold\Delta S_{CD} = q_{CD}/T_{\mathrm{cold}}.

    • Over one complete cycle, ΔScycle=0\Delta S_{\mathrm{cycle}} = 0 (state function returns to initial value), so ΔSAB=−ΔSCD\Delta S_{AB} = -\Delta S_{CD}.

  3. Carnot Efficiency

    ηCarnot=1−TcoldThot.\eta_{\mathrm{Carnot}} = 1 - \frac{T_{\mathrm{cold}}}{T_{\mathrm{hot}}}.
    • This is the maximum possible efficiency for any engine operating between two temperatures. It depends only on the reservoir temperatures.

  4. Direction of Spontaneous Heat Flow

    • Two subsystems at different temperatures inside an insulated boundary: dS=dUA(1/TA−1/TB)dS = dU_A(1/T_A - 1/T_B).

    • For dS≥0dS \ge 0 (second law), heat must flow from hot to cold (dUA<0dU_A < 0 when TA>TBT_A > T_B).

    • Equilibrium (dS=0dS = 0) is reached when TA=TBT_A = T_B.


Section 4.3: Microscopic View of Entropy

  1. Entropy Increases Until Equilibrium (Isolated Systems)

    • The second law for an isolated system: dS≥0dS \ge 0, with equality at equilibrium.

    • Entropy rises during spontaneous processes and reaches its maximum at equilibrium.

  2. The Clausius Inequality

    dS≥δqT.dS \ge \frac{\delta q}{T}.
    • Equality for reversible processes; strict inequality for irreversible processes.

    • Irreversibility produces additional entropy beyond the entropy carried by heat flow.

    • For an isolated system (δq=0\delta q = 0): reduces to dS≥0dS \ge 0.

  3. Boltzmann’s Formula (Microcanonical Ensemble)

    S=kBln⁡Ω,S = k_{\mathrm{B}} \ln \Omega,

    where Ω\Omega is the number of accessible microstates at fixed UU, VV, NN. The logarithm ensures entropy is extensive (additive for independent subsystems).

  4. Gibbs Entropy (General Probability Distribution)

    S=−kB∑ipiln⁡pi.S = -k_{\mathrm{B}} \sum_i p_i \ln p_i.
    • Reduces to Boltzmann’s formula when all Ω\Omega microstates are equally probable (pi=1/Ωp_i = 1/\Omega).

    • Applies to the canonical ensemble (pi=e−βEi/Qp_i = e^{-\beta E_i}/Q) and any other ensemble.

  5. Canonical Entropy Identity

    • Evaluating the Gibbs entropy with canonical probabilities yields

    S=UT+kBln⁡Q.S = \frac{U}{T} + k_{\mathrm{B}} \ln Q.
    • Directly ties the macroscopic state function SS to the partition function QQ from Chapter 2.

  6. Helmholtz Free Energy

    • Rearranging the canonical entropy identity:

    A≡U−TS=−kBTln⁡Q.A \equiv U - TS = -k_{\mathrm{B}}T\ln Q.
    • Natural variables of AA are TT and VV.

    • All canonical thermodynamic quantities (SS, UU, PP, CVC_V) can be derived from AA by differentiation.

    • Defining A=U−TSA = U - TS is the same Legendre-transform strategy used to define H=U+PVH = U + PV in Section 3.3: replace a hard-to-control variable (SS) with an easy-to-control one (TT).

  7. Microscopic Consistency

    • The Gibbs entropy depends only on probabilities {pi}\{p_i\}. Entropy changes when probabilities change (heat), not when energy levels shift (work).

    • This is consistent with the microscopic First Law from Section 3.2: δq=∑iEi dpi\delta q = \sum_i E_i\,dp_i and δw=∑ipi dEi\delta w = \sum_i p_i\,dE_i.


2. Checklist of Most Important Equations

Below is a unified list of the major equations from Sections 4.1–4.3.

A. Entropy Definition

dS=δqrevT,ΔS=∫ABδqrevT.dS = \frac{\delta q_{\mathrm{rev}}}{T}, \qquad \Delta S = \int_A^B \frac{\delta q_{\mathrm{rev}}}{T}.

B. Fundamental Thermodynamic Relation

dU=T dS−P dV.dU = T\,dS - P\,dV.

C. Entropy Change for an Ideal Gas (from VV and TT)

ΔS=∫T1T2CVT dT+NkBln⁡ ⁣(V2V1).\Delta S = \int_{T_1}^{T_2} \frac{C_V}{T}\,dT + Nk_{\mathrm{B}} \ln\!\left(\frac{V_2}{V_1}\right).

D. Carnot Efficiency

ηCarnot=1−TcoldThot.\eta_{\mathrm{Carnot}} = 1 - \frac{T_{\mathrm{cold}}}{T_{\mathrm{hot}}}.

E. Clausius Inequality

dS≥δqT.dS \ge \frac{\delta q}{T}.

F. Boltzmann Entropy

S=kBln⁡Ω.S = k_{\mathrm{B}} \ln \Omega.

G. Gibbs Entropy

S=−kB∑ipiln⁡pi.S = -k_{\mathrm{B}} \sum_i p_i \ln p_i.

H. Canonical Entropy Identity

S=UT+kBln⁡Q.S = \frac{U}{T} + k_{\mathrm{B}} \ln Q.

I. Helmholtz Free Energy

A=U−TS=−kBTln⁡Q.A = U - TS = -k_{\mathrm{B}}T \ln Q.