Heat Capacity Formula:
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Definition: Heat capacity is the amount of heat energy required to raise the temperature of a substance by one degree Kelvin.
Purpose: It helps in understanding how different materials absorb and store thermal energy, which is crucial in thermodynamics and material science.
The calculator uses the formula:
Where:
Explanation: The heat energy is divided by the temperature change to determine how much energy the substance can absorb per degree of temperature change.
Details: Heat capacity is crucial for designing thermal systems, understanding climate patterns, and developing materials with specific thermal properties.
Tips: Enter the heat energy in Joules and temperature change in Kelvin. Both values must be positive numbers.
Q1: What's the difference between heat capacity and specific heat capacity?
A: Heat capacity is an extensive property (depends on amount of substance), while specific heat capacity is intensive (per unit mass).
Q2: Can heat capacity be negative?
A: Normally no, except in very unusual thermodynamic systems. For most practical purposes, it's always positive.
Q3: How does heat capacity vary with temperature?
A: For most materials, heat capacity increases with temperature, especially near phase transitions.
Q4: What are typical heat capacity values?
A: Water has high heat capacity (about 4186 J/kg·K), while metals typically range from 200-900 J/kg·K.
Q5: Why use Kelvin instead of Celsius?
A: Kelvin is the absolute temperature scale required in thermodynamic calculations, though the size of 1K equals 1°C.