Analyze water vapor behavior with chemistry tools. Compare saturation pressure, dew point, and relative humidity. Use responsive inputs, graph trends, and export results instantly.
The page uses a single-column flow. The calculator fields switch to three columns on large screens, two on smaller screens, and one on mobile.
The chart shows the Buck saturation vapor pressure curve around the current working range. When available, the result point and actual pressure line are also displayed.
These sample values use the Buck saturation equation for water.
| Temperature (°C) | Saturation Vapor Pressure (kPa) | Saturation Vapor Pressure (mmHg) | Approx. Saturation Mole Fraction at 101.325 kPa |
|---|---|---|---|
| 0 | 0.61121 | 4.584452 | 0.00603217 |
| 10 | 1.22786 | 9.209709 | 0.01211804 |
| 25 | 3.168531 | 23.76594 | 0.03127097 |
| 40 | 7.38236 | 55.372251 | 0.07285822 |
| 60 | 19.945145 | 149.600894 | 0.19684328 |
| 80 | 47.410267 | 355.60625 | 0.46790296 |
| 100 | 101.307781 | 759.870849 | 0.99983006 |
es(T) = 0.61121 × exp[(18.678 − T/234.5) × T / (257.14 + T)]
Here, T is temperature in °C and es is saturation vapor pressure in kPa. This is the default broad-range model in the calculator.
log10(P) = A − B / (C + T)
The calculator uses standard water coefficients and converts the Antoine result from mmHg to kPa. This model is common in chemistry references.
e = (RH / 100) × es
RH = 100 × e / es
VPD = es − e
y = e / Ptotal
ρv = 216.7 × e(hPa) / T(K)
The dew point is obtained by numerically inverting the selected saturation relation until the saturation pressure equals the entered actual vapor pressure.
Water vapor pressure is the partial pressure created by gaseous water molecules. At saturation, it depends mainly on temperature for pure water.
Yes. Higher temperature gives water molecules more kinetic energy, so more molecules escape into the gas phase and vapor pressure rises.
Saturation vapor pressure is the maximum equilibrium value at a temperature. Actual vapor pressure is the real partial pressure currently present in the gas mixture.
Relative humidity compares actual vapor pressure with saturation vapor pressure. It tells you how close the air or gas mixture is to saturation.
Vapor pressure deficit is the gap between saturation and actual vapor pressure. It is useful when studying evaporation, drying, and gas-water equilibrium behavior.
Choose Buck for a practical broad-range estimate. Choose Antoine when you want a classic chemistry correlation within its coefficient temperature range.
It can appear above 100% during supersaturation, rapid cooling, condensation onset, or inconsistent inputs. The calculator flags this so you can review conditions.
No. Dissolved solutes reduce water activity and lower vapor pressure. This calculator is intended for pure water behavior unless you add solution corrections separately.
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.