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Thermal physics and thermodynamics

Physics (B.Sc) · Thermal physics · free study notes for exams, placements and interviews

In short

Thermal physics is the study of heat, temperature, work and the bulk properties of matter; thermodynamics is its macroscopic framework — four laws plus a set of state functions (U, H, S, F, G) that predict what a system can and cannot do without any knowledge of atoms. It fixes the ceiling on every engine, refrigerator, power plant and heat pump, and explains phase changes, gas liquefaction and thermal radiation. In B.Sc Physics it is a full paper; it is heavily examined in GATE (PH), IIT-JAM, CSIR-UGC NET, JEST and TIFR, and in state PSU and PSC technical papers. Employers who test it directly include BARC, ISRO, DRDO, CSIR-NPL, IMD, NTPC, BHEL, cryogenic and HVAC companies, and semiconductor/thermal-design teams.

Explained

Systems, state, equilibrium and the zeroth law

First law: energy, work, heat and specific heats

Second law, entropy and the Carnot cycle

Thermodynamic potentials, Maxwell relations and TdS equations

Real gases, liquefaction and the Joule–Thomson effect

Phase transitions, equilibrium and thermal radiation

Key points

Formulas and examples

First law: dU = δQ − δW, δW = P dV. U, H in J; P in Pa; V in m³; T in K.
Ideal gas: PV = nRT, R = 8.314 J mol⁻¹K⁻¹; C_P − C_V = R; γ = C_P/C_V.
Isothermal work (ideal gas): W = nRT ln(V₂/V₁); ΔU = 0, Q = W.
Reversible adiabatic: PVᵍ = const, TVᵍ⁻¹ = const, TP(1−γ)/γ = const; W = nR(T₁−T₂)/(γ−1).
Entropy of an ideal gas: ΔS = nC_V ln(T₂/T₁) + nR ln(V₂/V₁) = nC_P ln(T₂/T₁) − nR ln(P₂/P₁), in J/K.
Solid/liquid heating: ΔS = mc ln(T₂/T₁); phase change: ΔS = mL/T.
Carnot: η = 1 − T_C/T_H; COP_ref = T_C/(T_H − T_C); COP_hp = T_H/(T_H − T_C).
Clausius inequality: ∮ δQ/T ≤ 0. Entropy generation S_gen = ΔS_sys + ΔS_surr ≥ 0.
Potentials: H = U + PV; F = U − TS; G = H − TS; dG = −S dT + V dP.
Maxwell relations: (∂T/∂V)_S = −(∂P/∂S)_V; (∂T/∂P)_S = (∂V/∂S)_P; (∂S/∂V)_T = (∂P/∂T)_V; (∂S/∂P)_T = −(∂V/∂T)_P.
C_P − C_V = TVβ²/κ_T, β = (1/V)(∂V/∂T)_P in K⁻¹, κ_T = −(1/V)(∂V/∂P)_T in Pa⁻¹.
van der Waals: (P + an²/V²)(V − nb) = nRT; T_c = 8a/27Rb, P_c = a/27b², V_c = 3nb.
Joule–Thomson: μ_JT = (∂T/∂P)_H = (1/C_P)[T(∂V/∂T)_P − V]; inversion T_i = 2a/Rb.
Clausius–Clapeyron: dP/dT = L/[T(v₂ − v₁)]; L in J/kg, v in m³/kg, dP/dT in Pa/K.
Radiation: E = σT⁴; net P = eσA(T⁴ − T_s⁴); λ_max T = 2.898 × 10⁻³ m·K.
Fourier conduction: Q̇ = kA(T₁ − T₂)/L, k in W m⁻¹K⁻¹.

1. Carnot engine and the real-plant gap. Steam at 540 °C (813 K) rejecting to a condenser at 40 °C (313 K).

2. Reversible adiabatic expansion. 2 mol of a diatomic ideal gas (γ = 1.4) at 300 K expands reversibly and adiabatically to twice its volume.

3. Entropy generated by mixing hot and cold water. 200 g at 80 °C mixed with 300 g at 20 °C, c = 4,186 J kg⁻¹K⁻¹, insulated.

4. Clausius–Clapeyron: boiling point at altitude. Water at 100 °C: L_v = 2,257 kJ/kg, v_g = 1.673 m³/kg, v_l = 0.001 m³/kg.

5. Radiative loss from a hot surface. A furnace wall patch of 0.05 m², emissivity 0.8, at 500 K in a 300 K room.

QuantityNatural variablesMinimised / conserved whenTypical use
US, VIsolated system (S, V fixed)Energy balance, first law
HS, PConstant-P heating; conserved in throttlingEnthalpy of reaction, J–T effect
FT, VConstant T and VMax total work, statistical link
GT, PConstant T and PPhase and chemical equilibrium
ReversibleIrreversible
RateInfinitely slowFinite
∮δQ/T= 0< 0
S_gen0> 0
Work outputMaximumLess
ExampleIdealised Carnot cycleFree expansion, throttling, friction

Where it is used

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Related topics

Statistical mechanics basics · Kinetic theory of gases · Heat transfer: conduction, convection and radiation · Power cycles: Otto, Diesel, Rankine and Brayton · Blackbody radiation and quantum origins · Low-temperature physics and cryogenics

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