Specific Heat Capacity Formula:
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Definition: This equation calculates the amount of heat energy (Q) required to change the temperature of a substance based on its mass (m), specific heat capacity (c), and temperature change (ΔT).
Purpose: It helps in thermodynamics calculations for determining energy requirements in heating/cooling processes.
The equation is:
Where:
Explanation: The equation shows that heat energy required is directly proportional to mass, specific heat capacity, and temperature change.
Details: Specific heat capacity determines how much energy a substance can store per unit mass per degree of temperature change. It's crucial for designing heating/cooling systems.
Tips: Enter mass in kg, specific heat capacity (default 4186 J/kg·K for water), and temperature change in K. All values must be > 0.
Q1: What are typical specific heat capacity values?
A: Water = 4186 J/kg·K, Aluminum = 900 J/kg·K, Iron = 450 J/kg·K, Air ≈ 1000 J/kg·K.
Q2: Can I use Celsius instead of Kelvin?
A: Yes, because ΔT is the same in both scales (1°C change = 1K change).
Q3: Why is water's specific heat capacity important?
A: Water's high specific heat capacity makes it excellent for temperature regulation in nature and industrial processes.
Q4: How does specific heat relate to thermal conductivity?
A: They're different properties - specific heat measures energy storage, while conductivity measures energy transfer.
Q5: What if I need to calculate for cooling?
A: The same equation applies - just remember Q will be negative for cooling (heat energy removed).