Atmospheres to Kilopascals Converter
Common Conversions
| atm | kPa |
|---|---|
| 0.01 | 1.013 |
| 0.1 | 10.133 |
| 0.25 | 25.331 |
| 0.5 | 50.663 |
| 0.75 | 75.994 |
| 1 | 101.325 |
| 1.5 | 151.988 |
| 2 | 202.65 |
| 3 | 303.975 |
| 5 | 506.625 |
| 10 | 1013.25 |
| 20 | 2026.5 |
Why this conversion matters in chemistry
Atmospheres is the unit most people learn pressure in, but SI thermodynamics runs on kilopascals. A bomb calorimeter charged to 30 atm of oxygen is sitting at 3040 kPa, and that's the number you need once the gas constant in the calculation is R = 8.314 J/(mol·K) — because 1 kPa·L equals 1 J, so the units match up cleanly. Skipping the conversion is the fast way to an enthalpy value that's off by a quiet factor of 101. The arithmetic is one multiplication, but it's the difference between a calculation that makes sense and one that doesn't.
Formula
Worked Examples
The reference point. Sea-level atmospheric pressure, exact by international agreement.
1 bar — IUPAC's standard pressure since 1982, just barely below 1 atm. The difference is small enough to round away in most calculations, big enough to matter in precise thermodynamics.
Common line pressure downstream of a regulator on a teaching-lab gas cylinder.
Half an atmosphere. The regime where reduced-pressure work starts — low-boiling solvents begin distilling comfortably below this, while moderate-BP solvents on a rotovap usually sit lower still, around 0.1–0.2 atm.