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Adiabatic & Isothermal Process Calculator

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Understanding the adiabatic and isothermal process calculator — concept and principle

When a gas is compressed or expanded, the result depends on what happens to the heat. In an adiabatic process no heat is exchanged, so the gas heats up when compressed; in an isothermal process heat flows out so the temperature stays constant. Enter the initial pressure, the initial and final volumes, the starting temperature and the heat-capacity ratio γ, and the calculator gives the final pressure, temperature and work for both cases side by side.

Isothermal versus adiabatic compressionCompressing 10 L of air at 100 kPa to 2 L: isothermally 500 kPa at 300 K with 1.61 kJ of work; adiabatically 952 kPa and 571 K with 2.26 kJ.Squeeze 10 L down to 2 L, two ways10 L100 kPa300 KIsothermal: heat leaks outP₂ = 500 kPaT₂ = 300 Kwork 1.61 kJAdiabatic: no heat escapesP₂ = 952 kPaT₂ = 571 Kwork 2.26 kJPV¹·⁴ = const → 100 × 5¹·⁴ = 952 kPa
With no heat escaping, the gas heats to 571 K, so pressure and work end up higher.

How it is calculated

Pressures are in kPa and volumes in litres; since kPa × L = J, the work is divided by 1000 to give kJ. Positive work means work is done on the gas (compression).

The principle

The first law says ΔU = Q + W. With Q = 0, all work done on the gas goes into internal energy, so its temperature rises. For an ideal gas this leads to PV^γ = constant, where γ = c_p/c_v is about 1.4 for air and other diatomic gases near room temperature and 5/3 for monatomic gases. In the isothermal case ΔU = 0 for an ideal gas, so every joule of work leaves as heat, and PV stays constant. The adiabatic curve is steeper, which is why it needs more work for the same compression.

Worked example

  1. Inputs: P₁ = 100 kPa, V₁ = 10 L, V₂ = 2 L, T₁ = 300 K, γ = 1.4. Compression ratio V₁/V₂ = 5.
  2. Adiabatic P₂ = 100 × 5^1.4 = 100 × 9.51827 = 951.8269694 kPa.
  3. Adiabatic T₂ = 300 × 5^0.4 = 300 × 1.90365 = 571.0961816 K.
  4. Adiabatic work = (951.827 × 2 − 100 × 10) / 0.4 = 903.654 / 0.4 = 2259.13 J = 2.259134847 kJ.
  5. Isothermal P₂ = 100 × 10 / 2 = 500 kPa.
  6. Isothermal work = 100 × 10 × ln 5 = 1609.44 J = 1.609437912 kJ.
How Adiabatic P₂ (kPa) changes with γ (air 1.4)How Adiabatic P₂ changes with γ02,0004,0006,0008,00010,0000.350.71.051.41.752.12.8Example: 951.8269694γ (air 1.4)
Each point is the calculator re-run with only “γ (air 1.4)” changed; the gold point is the default example. Change the inputs above and this chart follows your numbers.
γ (air 1.4)Adiabatic P₂ (kPa)
0.35175.6465005
0.7308.5169314
1.05541.8991934
1.4951.8269694
1.751,671.850762
2.12,936.547358
2.89,059.745796

How to read the result

Compressing air five-fold without cooling almost doubles its absolute temperature, here from 27 °C to about 298 °C, and needs about 40% more work than the cooled isothermal case. Real compressors fall between the two, which is why multi-stage compressors use intercoolers. For expansion (V₂ larger than V₁) the work becomes negative: the gas does work on its surroundings and, adiabatically, cools down.

Common mistakes

Keep in mind: Both models assume an ideal gas and a slow, reversible process. Real fast compressions involve friction and heat leakage, and γ changes with temperature. Real machinery design needs measured data and a qualified engineer.

Frequently asked questions

Why does a bicycle pump get hot?

Rapid compression is close to adiabatic, so the work you do raises the air temperature, and friction adds more.

What γ should I use for other gases?

About 1.67 for helium and argon, about 1.4 for air, nitrogen and oxygen, and around 1.3 for carbon dioxide or steam.

Sources: Y. A. Çengel and M. A. Boles, Thermodynamics: An Engineering Approach, McGraw-Hill · P. Atkins and J. de Paula, Atkins' Physical Chemistry, Oxford University Press

Checked 8 Nov 2026. Standard textbook formulas in SI units, computed in your browser. For learning and estimates — real designs must follow your local codes and be checked by a qualified engineer.

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