Understand gas behavior beyond ideal assumptions quickly today. Enter any three values to compute safely. Get Z, interpret deviations, and download clean outputs instantly.
Choose what you want to solve for. Use consistent state variables for the same gas sample. This tool computes Z = PV/(nRT) and rearrangements of the same relation.
The compressibility factor relates real-gas behavior to the ideal-gas equation: PV = Z n R T. Rearranging gives:
Interpretation: Z ≈ 1 suggests near-ideal behavior, Z > 1 often indicates dominant repulsive effects, and Z < 1 often indicates dominant attractive effects.
These sample cases show typical magnitudes and how Z indicates deviation from ideal behavior.
| Case | Pressure (kPa) | Volume (L) | Amount (mol) | Temperature (K) | Z | Note |
|---|---|---|---|---|---|---|
| A | 101.325 | 22.414 | 1 | 273.15 | ~1.00 | Near-ideal reference conditions. |
| B | 500 | 20 | 1 | 300 | ~0.40 | Stronger attractive effects possible. |
| C | 5000 | 5 | 1 | 600 | ~5.01 | Repulsive effects may dominate. |
The compressibility factor, Z, is a dimensionless correction that links real-gas behavior to the ideal-gas relation. From PV = Z nRT, Z measures how observed pressure–volume–temperature data differ from an ideal prediction.
At low pressures and moderate temperatures, many gases have Z near 1 because molecular interactions are weak. As pressure increases or temperature decreases, attractions and repulsions matter and Z can move below or above 1.
Since R = 8.314462618 is used with SI units, converting pressure to Pa, volume to m³, and temperature to Kelvin keeps calculations consistent. Use absolute pressure; gauge values can shift results, especially near atmospheric conditions.
In many engineering checks, Z often falls roughly between 0.8 and 1.2 at moderate pressures, but compressed systems can deviate more. As a reference point, using P=101.325 kPa, n=1 mol, and T=273.15 K gives about 22.414 L when Z is close to 1. If Z is extreme, confirm volume and amount describe the same sample, and verify temperature is absolute.
Z improves density estimates through V = Z nRT/P. Once molar volume is corrected, density follows from molar mass divided by molar volume, or ρ = P·M/(ZRT) for molar mass M. This helps in storage sizing, flow calculations, and compression work estimates.
Z is frequently correlated with reduced pressure and reduced temperature based on critical properties, or estimated using equations of state. This calculator complements those methods by computing Z from measured state data or by back-solving a missing variable when Z is known.
Z is used in gas metering, pipeline sizing, vessel calculations, and process modeling. Reporting Z with P, V, n, and T improves traceability and helps decide whether ideal-gas assumptions are acceptable for a given margin. The export buttons create shareable CSV and PDF summaries for reports.
Common mistakes include mixing molar and total volume, entering Celsius directly, or using nonphysical values. If results look wrong, check absolute pressure, Kelvin temperature, and consistent sample definitions. When back-solving P, V, n, or T, ensure Z is positive and represents the same gas composition.
No. Z approaches 1 at low pressure and moderate temperature, but can deviate strongly at high pressure, low temperature, or near saturation where molecular interactions matter.
Z < 1 often suggests attractive forces dominate, making the gas more compressible than ideal at the same conditions. It commonly appears at moderate pressures and relatively low temperatures.
Z > 1 often suggests repulsive effects dominate, making the gas less compressible than ideal. This can occur at higher pressures and higher densities.
Yes. Use absolute pressure for thermodynamic equations. Using gauge pressure can distort Z, especially near atmospheric pressure where the offset is large relative to the value.
Yes. Select the variable to solve for, then enter the remaining known variables. When solving for P, V, n, or T, you must also provide a positive Z value.
The relation requires absolute temperature. Kelvin keeps proportionality correct. Entering Celsius directly shifts the scale and can produce incorrect Z or state-variable results.
Recheck units and magnitudes, confirm volume corresponds to the same amount n, ensure pressure is absolute, and verify temperature is physically valid. Then recalculate using consistent inputs.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.