Heat Transfer Equation:
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Heat transfer by temperature change refers to the amount of thermal energy gained or lost by a substance when its temperature changes. This fundamental concept in thermodynamics is governed by the equation Q = m × c × ΔT, where thermal energy transfer is proportional to mass, specific heat capacity, and temperature change.
The calculator uses the heat transfer equation:
Where:
Explanation: The equation calculates the thermal energy required to change the temperature of a given mass of substance by a specific amount, depending on the material's ability to store heat (specific heat capacity).
Details: Accurate heat transfer calculations are essential for designing heating and cooling systems, understanding thermal processes in engineering, calculating energy requirements in chemical reactions, and analyzing thermal management in various applications from electronics to building design.
Tips: Enter mass in kilograms, specific heat capacity in J/kg·K, and temperature change in kelvin. Positive ΔT indicates temperature increase (heat gained), negative ΔT indicates temperature decrease (heat lost). All values must be valid (mass > 0, specific heat > 0).
Q1: What is specific heat capacity?
A: Specific heat capacity is the amount of heat energy required to raise the temperature of 1 kilogram of a substance by 1 kelvin. Different materials have different specific heat capacities.
Q2: Can temperature change be negative?
A: Yes, negative temperature change indicates cooling, meaning the substance loses heat energy to its surroundings.
Q3: Why use kelvin for temperature change?
A: Kelvin is used because it's an absolute temperature scale where 1 K change equals 1°C change, but kelvin avoids negative values in calculations.
Q4: What are typical specific heat values?
A: Water: 4184 J/kg·K, Aluminum: 897 J/kg·K, Iron: 449 J/kg·K, Copper: 385 J/kg·K. Water has one of the highest specific heat capacities.
Q5: How does this relate to phase changes?
A: This equation applies only to temperature changes without phase transitions. For phase changes (melting, boiling), latent heat equations are used instead.