Thermodynamics Formula Sheet

Thermodynamics Formula Sheet

All Key Equations in One Place — For Quick Revision & Exam Preparation

Last Updated: March 2026

📌 How to Use This Sheet

  • This page collects every important thermodynamics formula in one place, organised by topic.
  • Each formula includes all variables defined with SI units.
  • Use this for last-minute revision before GATE, ESE, or university exams — not as a substitute for understanding concepts.
  • For detailed explanations and worked examples, click the topic links to visit the full concept page.
  • ⚠️ All temperatures in thermodynamic formulas must be in Kelvin unless stated otherwise.

1. Laws of Thermodynamics

Zeroth Law

If A is in thermal equilibrium with C, and B is in thermal equilibrium with C, then A is in thermal equilibrium with B. (Defines temperature.)

First Law — Closed System

Q = ΔU + W

Q = heat added (J), ΔU = change in internal energy (J), W = work done by system (J)

For a cycle: Qnet = Wnet (since ΔU = 0)

Second Law

ΔSuniverse = ΔSsystem + ΔSsurroundings ≥ 0

Clausius Inequality: ∮ δQ/T ≤ 0

2. Ideal Gas Equations

Equation of State

PV = nRT (molar form)

PV = mRsT (mass form, Rs = R/M)

R = 8.314 J/(mol·K), Rs,air = 287 J/(kg·K)

Specific Heat Relations

Cp − Cv = R (Mayer’s relation)

γ = Cp / Cv (ratio of specific heats)

For air: Cp = 1.005 kJ/kg·K, Cv = 0.718 kJ/kg·K, γ = 1.4

Internal Energy & Enthalpy (Ideal Gas)

ΔU = nCvΔT (always, for ideal gas)

ΔH = nCpΔT (always, for ideal gas)

Isentropic (Adiabatic Reversible) Relations

TVγ−1 = constant

TP(1−γ)/γ = constant

PVγ = constant

3. Work in Common Processes (Closed System, Ideal Gas)

ProcessWork Done by Gas (W)
Isochoric (V = const)W = 0
Isobaric (P = const)W = PΔV = P(V&sub2; − V&sub1;)
Isothermal (T = const)W = nRT ln(V&sub2;/V&sub1;) = nRT ln(P&sub1;/P&sub2;)
Isentropic/AdiabaticW = (P&sub1;V&sub1; − P&sub2;V&sub2;)/(γ − 1) = nCv(T&sub1; − T&sub2;)
Polytropic (PVn = C)W = (P&sub1;V&sub1; − P&sub2;V&sub2;)/(n − 1)

4. Entropy Formulas

General Definition

dS = δQrev / T

Ideal Gas Entropy Change

ΔS = nCv ln(T&sub2;/T&sub1;) + nR ln(V&sub2;/V&sub1;)

ΔS = nCp ln(T&sub2;/T&sub1;) − nR ln(P&sub2;/P&sub1;)

Phase Change

ΔS = mL / T

L = latent heat (kJ/kg), T = phase change temperature (K)

Entropy Generation (Heat Transfer Across ΔT)

Sgen = Q(1/TL − 1/TH)

5. Enthalpy Formulas

Definition

H = U + PV, specific: h = u + Pv

Constant Pressure

QP = ΔH

Wet Steam

h = hf + x·hfg

x = dryness fraction (quality), hf = saturated liquid, hfg = latent heat

6. Power Cycle Efficiencies

General Heat Engine Efficiency

η = Wnet/QH = 1 − QL/QH

Carnot Cycle

ηCarnot = 1 − TL/TH

Maximum possible efficiency between temperatures TH and TL (in Kelvin)

Otto Cycle (Petrol Engine)

ηOtto = 1 − 1/r(γ−1)

r = compression ratio, γ = Cp/Cv

Diesel Cycle

ηDiesel = 1 − [1/r(γ−1)] × [(ργ − 1) / γ(ρ − 1)]

r = compression ratio, ρ = cut-off ratio = V&sub3;/V&sub2;

Dual Cycle (Mixed)

ηDual = 1 − [1/r(γ−1)] × [(rp·ργ − 1) / (rp − 1 + γ·rp(ρ − 1))]

rp = pressure ratio during constant-V heat addition

Rankine Cycle (Steam Power Plant)

ηRankine = [(h&sub1; − h&sub2;) − (h&sub4; − h&sub3;)] / (h&sub1; − h&sub4;)

h values from steam tables. Pump work: Wpump = h&sub4; − h&sub3; ≈ vf(P&sub4; − P&sub3;)

Brayton Cycle (Gas Turbine)

ηBrayton = 1 − 1/rp(γ−1)/γ

rp = pressure ratio = P&sub2;/P&sub1;

7. Refrigeration & Heat Pump

Coefficient of Performance — Refrigerator

COPR = QL/W = QL/(QH − QL)

Carnot: COPR,Carnot = TL/(TH − TL)

Coefficient of Performance — Heat Pump

COPHP = QH/W = QH/(QH − QL)

Carnot: COPHP,Carnot = TH/(TH − TL)

COPHP = COPR + 1

8. Steady Flow Energy Equation (SFEE)

General Form

Q − W = ˙m[(h&sub2; − h&sub1;) + (V&sub2;² − V&sub1;²)/2 + g(z&sub2; − z&sub1;)]

DeviceSimplified SFEE
Turbine/CompressorW = ˙m(h&sub1; − h&sub2;)
Heat ExchangerQ = ˙m(h&sub2; − h&sub1;)
Nozzle/Diffuserh&sub1; + V&sub1;²/2 = h&sub2; + V&sub2;²/2
Throttling Valveh&sub1; = h&sub2; (isenthalpic)

9. Heat Transfer Formulas

Conduction (Fourier’s Law)

Q = kA(T&sub1; − T&sub2;)/L

k = thermal conductivity (W/m·K), A = area (m²), L = thickness (m)

Thermal resistance: R = L/(kA)

Convection (Newton’s Law of Cooling)

Q = hA(Ts − T)

h = convection coefficient (W/m²·K)

Radiation (Stefan-Boltzmann Law)

Q = εσA(Ts&sup4; − Tsurr&sup4;)

ε = emissivity (0–1), σ = 5.67 × 10−8 W/(m²·K&sup4;), T in Kelvin

10. Important Constants

ConstantSymbolValueUnit
Universal Gas ConstantR8.314J/(mol·K)
Specific Gas Constant (Air)Rs287J/(kg·K)
Stefan-Boltzmann Constantσ5.67 × 10−8W/(m²·K&sup4;)
Boltzmann ConstantkB1.381 × 10−23J/K
Standard Atmospheric PressurePatm101.325kPa
Absolute Zero0 K = −273.15°C
Cp of AirCp1.005kJ/(kg·K)
Cv of AirCv0.718kJ/(kg·K)
γ for Airγ1.4
Gravitational Accelerationg9.81m/s²

Temperature Conversion Quick Reference

K = °C + 273.15

°F = (9/5) × °C + 32

°C = (5/9) × (°F − 32)

ΔT in K = ΔT in °C (temperature differences are the same in both scales)