Ideal Gas Law Equation:
From: | To: |
The ideal gas law equation P = ρRT/M calculates air pressure by relating pressure to air density, temperature, gas constant, and molar mass. This formula is derived from the fundamental ideal gas law and is widely used in atmospheric science and engineering applications.
The calculator uses the ideal gas law equation:
Where:
Explanation: The equation shows that air pressure is directly proportional to both density and temperature, and inversely proportional to molar mass.
Details: Accurate air pressure calculation is essential for weather forecasting, aviation, HVAC system design, and understanding atmospheric phenomena. It helps predict weather patterns, determine altitude, and design efficient ventilation systems.
Tips: Enter air density in kg/m³, temperature in Kelvin, molar mass in kg/mol (default is 0.02897 for dry air), and gas constant in J/mol·K (default is 8.314). All values must be positive numbers.
Q1: What is the standard value for molar mass of air?
A: The molar mass of dry air is approximately 0.02897 kg/mol. This value may vary slightly with humidity and composition.
Q2: Why use Kelvin instead of Celsius for temperature?
A: Kelvin is an absolute temperature scale where 0K represents absolute zero, making it appropriate for gas law calculations that involve temperature ratios.
Q3: What is the universal gas constant value?
A: The universal gas constant R is approximately 8.314 J/mol·K. This value is constant for all ideal gases.
Q4: How does humidity affect air pressure calculations?
A: Humid air has slightly lower density than dry air at the same temperature and pressure, which may affect precise calculations.
Q5: What are typical air pressure values at sea level?
A: Standard atmospheric pressure at sea level is approximately 101,325 Pascals (101.325 kPa).