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)
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)
| Process | Work 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/Adiabatic | W = (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)
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;)]
| Device | Simplified SFEE |
|---|---|
| Turbine/Compressor | W = ˙m(h&sub1; − h&sub2;) |
| Heat Exchanger | Q = ˙m(h&sub2; − h&sub1;) |
| Nozzle/Diffuser | h&sub1; + V&sub1;²/2 = h&sub2; + V&sub2;²/2 |
| Throttling Valve | h&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
| Constant | Symbol | Value | Unit |
|---|---|---|---|
| Universal Gas Constant | R | 8.314 | J/(mol·K) |
| Specific Gas Constant (Air) | Rs | 287 | J/(kg·K) |
| Stefan-Boltzmann Constant | σ | 5.67 × 10−8 | W/(m²·K&sup4;) |
| Boltzmann Constant | kB | 1.381 × 10−23 | J/K |
| Standard Atmospheric Pressure | Patm | 101.325 | kPa |
| Absolute Zero | — | 0 K = −273.15°C | — |
| Cp of Air | Cp | 1.005 | kJ/(kg·K) |
| Cv of Air | Cv | 0.718 | kJ/(kg·K) |
| γ for Air | γ | 1.4 | — |
| Gravitational Acceleration | g | 9.81 | m/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)