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Air Conditioner Cooling Capacity Calculation

Cooling Capacity Formula:

\[ Capacity = CFM \times 1.08 \times \Delta T \]

CFM
°F

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1. What is Air Conditioner Cooling Capacity?

Cooling capacity refers to the amount of heat energy an air conditioning system can remove from a space per hour, measured in BTU/hr (British Thermal Units per hour). It is a critical parameter for sizing HVAC systems appropriately.

2. How Does the Calculator Work?

The calculator uses the cooling capacity formula:

\[ Capacity = CFM \times 1.08 \times \Delta T \]

Where:

Explanation: The formula calculates the heat removal capacity based on the volume of air being moved and the temperature difference between supply and return air.

3. Importance of Cooling Capacity Calculation

Details: Proper cooling capacity calculation ensures efficient HVAC system operation, prevents undersizing (inadequate cooling) or oversizing (short cycling and poor humidity control), and optimizes energy consumption.

4. Using the Calculator

Tips: Enter CFM (air flow rate) and temperature difference in °F. Both values must be positive numbers. The calculator will compute the cooling capacity in BTU/hr.

5. Frequently Asked Questions (FAQ)

Q1: What is the significance of the 1.08 constant?
A: The constant 1.08 accounts for the specific heat of air (0.24 BTU/lb·°F) and standard air density (0.075 lb/ft³), converted to appropriate units for the calculation.

Q2: How do I measure CFM in practice?
A: CFM can be measured using an anemometer or calculated from duct size and air velocity. Professional HVAC technicians use specialized equipment for accurate measurements.

Q3: What is a typical ΔT for residential AC systems?
A: Most residential systems operate with a ΔT of 15-20°F between return and supply air when functioning properly.

Q4: Can this formula be used for heating calculations?
A: Yes, the same formula applies for heating capacity calculation, as it represents the heat transfer capacity of air movement.

Q5: How does altitude affect the calculation?
A: At higher altitudes, air density decreases, which may require adjustment of the constant factor for precise calculations.

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