Partial Pressure Calculator

Calculate partial pressures of gases in mixtures using Dalton's law, mole fractions, vapor pressure corrections, and real gas adjustments.

Gas Components (mole/volume %)

Total Pressure (at depth)
1.0000 atm
Surface pressure
Total (atm)
1.0000 atm
Total absolute pressure in atmospheres
Total (mmHg)
760.0 mmHg
Total pressure in millimeters of mercury
P(N₂)
0.7811 atm
Mole fraction: 0.7811 — partial pressure of N₂
P(O₂)
0.2096 atm
Mole fraction: 0.2096 — partial pressure of O₂
P(Ar)
0.0093 atm
Mole fraction: 0.0093 — partial pressure of Ar

Partial Pressure Breakdown

N₂
0.7811 atm
O₂
0.2096 atm
Ar
0.0093 atm

Component Breakdown

GasMole %Mole FractionP (atm)P (atm)P (mmHg)
N₂78.11%0.78110.78110.7811593.7
O₂20.96%0.20960.20960.2096159.3
Ar0.93%0.00930.00930.00937.1
Total99.97%1.00001.00001.0000760.0

Physiological Thresholds

ConditionPO₂ (atm)Status
Hypoxia (loss of consciousness)0.1✅ Safe
Normal sea level0.21PO₂ = 0.210 atm
Enriched air (safe)1.4⚠️ Risk
O₂ toxicity threshold1.6✅ Safe
CNS toxicity risk2✅ Safe
Planning notes, formulas, and examples

About the Partial Pressure Calculator

Dalton's law of partial pressures states that the total pressure of a gas mixture equals the sum of the partial pressures of each individual gas component. Each gas's partial pressure equals its mole fraction multiplied by the total pressure: Pᵢ = xᵢ × P_total. This fundamental principle is essential in chemistry, engineering, biology, and atmospheric science.

Understanding partial pressures is critical for: respiratory physiology (oxygen delivery to tissues depends on PO₂, not total pressure), diving safety (partial pressures of O₂ and N₂ determine toxicity risks at depth), industrial gas processing (distillation, absorption, membrane separations), and atmospheric chemistry (pollutant concentrations, greenhouse gas levels).

This calculator handles gas mixtures with up to 8 components, automatically calculates mole fractions and partial pressures from either moles or volume percentages, and provides context for common applications like breathing gases, atmospheric composition, and industrial processes. It includes altitude-adjusted atmospheric calculations and dissolved gas concentrations via Henry's law.

When This Page Helps

This calculator quickly determines partial pressures in complex gas mixtures, converts between pressure units, and applies physiological/safety context — invaluable for lab work, diving planning, medical gas calculations, and atmospheric chemistry.

How to Use the Inputs

  1. Enter the total pressure of the gas mixture (in atm, kPa, mmHg, or psi).
  2. Add gas components with either their mole amounts or volume/mole percentages.
  3. Use presets for common mixtures: dry air, exhaled breath, natural gas, etc.
  4. Review partial pressures for each component in your chosen pressure unit.
  5. Optionally enter altitude or depth to see adjusted pressures.
  6. Check the dissolved concentration using Henry's law constants.
  7. Compare results against physiological or safety thresholds.
Formula used
Dalton's Law: P_total = Σ Pᵢ = Σ (xᵢ × P_total), where xᵢ = nᵢ/n_total is the mole fraction. For ideal gases, the volume fraction equals the mole fraction. Henry's Law: C = k_H × P, where C = dissolved concentration, k_H = Henry's constant.

Example Calculation

Result: PO₂ = 0.2095 atm = 159.2 mmHg

In dry air at 1 atm: PO₂ = 0.2095 × 1.0 = 0.2095 atm = 159.2 mmHg. This is the inspired oxygen partial pressure at sea level.

Tips & Best Practices

  • For humid gas mixtures, subtract water vapor pressure from total pressure before calculating dry gas partial pressures.
  • At body temperature (37°C), water vapor pressure is 47 mmHg — always account for this in respiratory calculations.
  • Mole fraction equals volume fraction ONLY for ideal gases at the same T and P.
  • For breathing gas calculations, multiply PO₂ by the respiratory quotient to estimate alveolar partial pressures.
  • When collecting gases over water, subtract the vapor pressure of water to get the dry gas pressure.
  • Henry's law constants are highly temperature-dependent — always use values at your actual temperature.

Dalton's Law in Atmospheric Chemistry

Earth's atmosphere is a natural example of Dalton's law. The total atmospheric pressure at sea level (~101.325 kPa) is the sum of partial pressures from nitrogen (79.1 kPa), oxygen (21.2 kPa), argon (0.94 kPa), carbon dioxide (0.04 kPa), and trace gases. Weather reporting of barometric pressure reflects this sum. Changes in water vapor content alter the total pressure and shift the partial pressures of other components.

Breathing and Physiology

In medicine and diving, partial pressures determine gas exchange rates. Oxygen diffuses from alveoli into blood because alveolar PO₂ (~100 mmHg) exceeds venous PO₂ (~40 mmHg). At altitude, reduced PO₂ triggers hyperventilation and eventual acclimatization through increased red blood cell production. Hyperbaric oxygen therapy exploits elevated PO₂ to enhance wound healing and treat decompression sickness.

Industrial Gas Processing

Chemical engineers use partial pressures extensively in vapor-liquid equilibrium calculations (Raoult's law, modified Raoult's law), absorption column design, and membrane separation modeling. The driving force for gas absorption into a liquid is the difference between the gas-phase partial pressure and the equilibrium partial pressure above the liquid — directly connecting Dalton's law with Henry's law and mass transfer operations.

Sources & Methodology

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Frequently Asked Questions

  • The pressure that each gas in a mixture would exert if it alone occupied the entire volume at the same temperature. It's proportional to the gas's mole fraction.