Air Density Formula:
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Definition: This calculator computes the density of air based on pressure, temperature, and the specific gas constant for air.
Purpose: It helps engineers, meteorologists, and scientists determine air density for various applications in aerodynamics, HVAC, and atmospheric studies.
The calculator uses the formula:
Where:
Explanation: The pressure is divided by the product of the gas constant and temperature to obtain the air density.
Details: Air density affects aircraft performance, wind load calculations, ventilation systems, and weather forecasting. It decreases with increasing temperature and altitude.
Tips: Enter the pressure in Pascals (default 101325 Pa for sea level), temperature in Kelvin (default 293.15K or 20°C), and gas constant (default 287 J/kg·K for dry air). All values must be > 0.
Q1: What's standard air density at sea level?
A: Approximately 1.225 kg/m³ at 15°C (288.15K) and 101325 Pa.
Q2: How does temperature affect air density?
A: Warmer air is less dense. Density decreases by about 1% for every 3°C increase in temperature.
Q3: When would I change the gas constant value?
A: Use 287 J/kg·K for dry air. For humid air, use a slightly lower value (285-286 J/kg·K).
Q4: How do I convert Celsius to Kelvin?
A: Add 273.15 to the Celsius temperature (e.g., 20°C = 293.15K).
Q5: Does this calculator account for humidity?
A: No, this calculates dry air density. For moist air, more complex equations are needed.