Heat Equation:
From: | To: |
The heat equation (Q = m × Cp × ΔT) calculates the amount of heat energy transferred when the temperature of a substance changes. It's fundamental in thermodynamics and heat transfer calculations.
The calculator uses the heat equation:
Where:
Explanation: The equation shows that heat transfer is proportional to the mass of the substance, its specific heat capacity, and the temperature change it undergoes.
Details: Calculating heat transfer is essential for designing heating/cooling systems, understanding thermal processes in engineering, and solving problems in physics and chemistry.
Tips: Enter mass in kilograms, specific heat capacity in J/kg·K, and temperature change in Kelvin. All values must be valid (mass > 0, Cp > 0).
Q1: What are typical Cp values?
A: Water has Cp ≈ 4186 J/kg·K, while metals typically range from 385-900 J/kg·K. Air at room temperature is about 1005 J/kg·K.
Q2: Why use Kelvin for temperature change?
A: A 1°C change equals a 1K change, but Kelvin is used in thermodynamics because it's an absolute scale with no negative values.
Q3: Can I use this for phase changes?
A: No, this equation only works for temperature changes. Phase changes require the latent heat equation (Q = mL).
Q4: What if my substance is cooling?
A: The equation still works - ΔT will be negative (final minus initial temperature), giving a negative Q indicating heat loss.
Q5: How accurate is this calculation?
A: It's accurate for most purposes, but Cp can vary slightly with temperature for some materials.