PHYSICAL CHEMISTRYGas Laws & PressureChemistry Calculator
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Water Vapor Pressure & Humidity

Water vapor pressure is the partial pressure of water vapor in equilibrium with liquid water. The Buck equation P = 0.61121 × e^((18.678 - T/234.5) × T/(257.14+T)) is highly accurate for 0–100°C. Essential for humidity, dew point, and meteorological calculations.

Concept Fundamentals
Most accurate 0–100°C
Buck Formula
log P = A - B/(C+T)
Antoine
RH = P/P_sat × 100%
Humidity
T when P = P_sat
Dew Point
Calculate Water Vapor PressureBuck | Antoine | Magnus | Tetens

Why This Chemistry Calculation Matters

Why: Water vapor pressure underpins humidity calculations, dew point determination, HVAC design, and weather forecasting. Critical for food preservation and environmental science.

How: Enter temperature; the calculator applies Buck (most accurate), Antoine, Magnus, and Tetens formulas. Buck typically has error <0.01% for 0–100°C.

  • Buck formula is most accurate for typical atmospheric temperatures.
  • Relative humidity RH = (actual P / saturation P) × 100%.
  • Dew point is the temperature at which air becomes saturated.

Water Vapor Pressure Examples

❄️ Water at 0°C

Vapor pressure at freezing point

🌡️ Water at 25°C

Room temperature vapor pressure

💧 Water at 50°C

Moderate temperature

🔥 Water at 80°C

Near boiling point

💨 Water at 100°C

Boiling point at 1 atm

🌊 Water at 20°C

Standard room temperature

☀️ Water at 30°C

Warm day temperature

🌡️ Water at 40°C

Hot day temperature

🔥 Water at 60°C

Hot water temperature

💨 Water at 90°C

Very near boiling

❄️ Water at 10°C

Cool temperature

🧊 Water at 5°C

Near freezing

🌤️ Water at 15°C

Mild temperature

☀️ Water at 35°C

Body temperature range

🔥 Water at 75°C

Hot water

Calculate Water Vapor Pressure

⚠️For educational and informational purposes only. Verify with a qualified professional.

🔬 Chemistry Facts

📊

Buck formula error typically <0.01% for 0–100°C.

— NIST

🌡️

At 25°C: P_sat ≈ 3.17 kPa (23.8 mmHg).

— NIST

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At 100°C: P_sat = 101.325 kPa (boiling at 1 atm).

— IUPAC

🌦️

RH = 100% at dew point; condensation begins.

— WMO

What is Water Vapor Pressure?

Water vapor pressure is the partial pressure of water vapor in the atmosphere. It represents the pressure exerted by water molecules in the gas phase when in equilibrium with liquid water at a given temperature. This is crucial for understanding humidity, cloud formation, and weather patterns.

Key Values
0°C: 0.611 kPa (4.58 mmHg)
25°C: 3.17 kPa (23.8 mmHg)
100°C: 101.325 kPa (760 mmHg)

Water Vapor Pressure Table

Temperature (°C)Temperature (°F)Vapor Pressure (kPa)Vapor Pressure (mmHg)Vapor Pressure (atm)
0320.61124.58450.0060
5410.87246.54390.0086
10501.22799.20970.0121
15591.705212.78990.0168
20682.338317.53900.0231
25773.168523.76600.0313
30864.245131.84110.0419
35955.626842.20420.0555
401047.382455.37240.0729
5012212.349492.62840.1219
6014019.9451149.60130.1968
7015831.2010234.02720.3079
8017647.4103355.60720.4679
9019470.1521526.18580.6923
100212101.3078759.87290.9998

Key Concepts

Relative Humidity

RH = (Actual vapor pressure / Saturation vapor pressure) × 100%. When RH = 100%, condensation occurs.

Dew Point

The temperature at which air becomes saturated with water vapor and condensation begins to form.

Saturation

When vapor pressure equals saturation vapor pressure, the air is at 100% relative humidity.

How Do Water Vapor Pressure Formulas Work?

Multiple empirical and theoretical formulas exist to calculate water vapor pressure. Each has different accuracy ranges and applications. The Buck formula is generally most accurate for typical temperatures (0-100°C).

🔬 Antoine Equation

log₁₀(P) = A - B/(C + T)

0-100°C: A=8.07131, B=1730.63, C=233.426

100-374°C: A=8.14019, B=1810.94, C=244.485

Most accurate for high temperatures (>100°C)

📊 Buck Formula (Arden Buck)

P = 0.61121 × e^((18.678 - T/234.5) × T/(257.14+T))

Most accurate for 0-100°C range

Error typically <0.01% in typical conditions

🌡️ Magnus Formula

P = 0.61094 × e^(17.625×T/(T+243.04))

Good accuracy for 0-50°C

Commonly used in meteorology

💧 Tetens Formula

P = 0.61078 × e^(17.27×T/(T+237.3))

Similar to Magnus, good for 0-50°C

Used in agricultural and environmental applications

When to Use Water Vapor Pressure Calculations

Water vapor pressure calculations are essential in meteorology, HVAC design, food preservation, and many other fields.

🌦️

Meteorology

Calculate humidity, dew point, and predict weather patterns including cloud formation and precipitation.

  • Weather forecasting
  • Humidity calculations
  • Dew point determination
🏠

HVAC Systems

Design heating, ventilation, and air conditioning systems with proper humidity control.

  • Humidity control
  • Condensation prevention
  • Comfort calculations
🍔

Food Preservation

Optimize drying processes, predict spoilage, and design food storage systems.

  • Freeze-drying
  • Dehydration
  • Shelf life prediction

Water Vapor Pressure Formulas Comparison

Accuracy Comparison (0-100°C)

Buck Formula: Most accurate, error <0.01%

Antoine Equation: Very accurate, especially >100°C

Tetens Formula: Good for 0-50°C, error ~0.05%

Magnus Formula: Good for 0-50°C, error ~0.06%

Simple Formula: Less accurate, error ~1-7%

Practical Water Vapor Pressure Examples

Example: Room Temperature

Given:

  • Temperature: 25°C
  • Calculate vapor pressure

Solution (Buck):

P = 0.61121 × e^((18.678 - 25/234.5) × 25/(257.14+25))

P = 3.169 kPa (23.8 mmHg)

Example: Boiling Point

Given:

  • Temperature: 100°C
  • Atmospheric pressure: 101.325 kPa

Solution:

At 100°C, vapor pressure equals atmospheric pressure

P = 101.325 kPa (760 mmHg)

This is why water boils at 100°C at sea level

Limitations and Considerations

⚠️ When Calculations May Not Apply

  • • Very high pressures (non-ideal behavior)
  • • Near critical point (374°C, 22.1 MPa)
  • • Saltwater or solutions (lower vapor pressure)
  • • Temperature ranges outside formula validity
  • • Non-equilibrium conditions

✓ Assumptions Made

  • • Pure water (no dissolved substances)
  • • Equilibrium conditions
  • • Standard atmospheric composition
  • • Flat surface (no curvature effects)
  • • Temperature is uniform

📚 Official Data Sources

⚠️ Disclaimer: This calculator uses empirical formulas (Antoine, Buck, Magnus, Tetens) for water vapor pressure. For precise work consult NIST Steam Tables, IAPWS-IF97 for water properties, and IUPAC Gold Book for thermodynamic definitions.

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