Estimate oxygen pressure at elevation with humidity corrections. Compare dry, inspired, and alveolar values using practical chemistry calculations today.
The chart compares dry oxygen pressure, inspired oxygen pressure, and estimated alveolar oxygen pressure from sea level to 10,000 meters.
| Altitude | Barometric Pressure (kPa) | Dry PO₂ (kPa) | Inspired PO₂ (kPa) | Estimated Alveolar PO₂ (kPa) |
|---|---|---|---|---|
| 0 m | 101.325 | 21.228 | 19.913 | 13.288 |
| 1,500 m | 84.556 | 17.715 | 16.400 | 9.775 |
| 3,000 m | 70.109 | 14.688 | 13.373 | 6.748 |
| 4,500 m | 57.729 | 12.094 | 10.780 | 4.155 |
| 6,000 m | 47.182 | 9.885 | 8.570 | 1.945 |
1) Barometric pressure at altitude
For the troposphere, pressure decreases with altitude using the barometric relation:
P = P₀ × (1 − Lh/T₀)^(gM/RL)
2) Dry oxygen partial pressure
PO₂(dry) = FIO₂ × P
3) Humid ambient oxygen pressure
PO₂(humid ambient) = FIO₂ × (P − PH₂O,ambient)
4) Inspired oxygen after airway humidification
PIO₂ = FIO₂ × (P − PH₂O,body)
5) Estimated alveolar oxygen
PAO₂ = PIO₂ − (PaCO₂ / RQ)
These formulas help estimate oxygen availability as elevation rises. The airway humidification adjustment is important because water vapor displaces part of the inspired gas pressure.
It estimates oxygen partial pressure at altitude using atmospheric pressure, oxygen fraction, humidity, body vapor pressure, and an alveolar gas approximation.
The oxygen percentage in dry air stays nearly constant, but total atmospheric pressure decreases. Because partial pressure depends on total pressure, oxygen pressure falls as altitude rises.
Dry oxygen pressure uses total barometric pressure only. Inspired oxygen pressure subtracts body water vapor pressure because inhaled air becomes fully humidified in the airways.
Humidity slightly changes ambient gas composition. It matters more for precise gas calculations, especially when comparing dry air values with real inhaled air conditions.
It estimates oxygen pressure in the alveoli after accounting for carbon dioxide and respiratory quotient. It is useful for physiology-based approximations, not diagnosis.
Use 101.325 kPa for standard atmosphere. For more realism, enter your local sea-level adjusted pressure from meteorological observations or lab conditions.
Yes. Change the oxygen fraction input to evaluate enriched breathing gas conditions. The formulas scale the oxygen partial pressure directly from that fraction.
No. It is an educational chemistry and gas-law tool. Medical interpretation requires clinical context, measurements, and guidance from qualified professionals.